Oregon Explorer CrossSearch Search Results

1501. [Image] An Act to Authorize the Bureau of Reclamation to Conduct Certain Feasibility Studies to Augment Water Supplies for the Klamath Project, Oregon and California, and for Other Purposes


	"Nov. 9, 2000, (S. 2882)."; "114 Stat. 2221."; "Public Law 106-498."
	Citation Citation Citation Abstract Copy Title: An Act to Authorize the Bureau of Reclamation to Conduct Certain Feasibility Studies to Augment Water Supplies for the Klamath Project, Oregon and California, and for Other Purposes Author: United States Year: 2000, 2005 "Nov. 9, 2000, (S. 2882)."; "114 Stat. 2221."; "Public Law 106-498." Title: An Act to Authorize the Bureau of Reclamation to Conduct Certain Feasibility Studies to Augment Water Supplies for the Klamath Project, Oregon and California, and for Other Purposes Author: United States Year: 2000, 2005 "Nov. 9, 2000, (S. 2882)."; "114 Stat. 2221."; "Public Law 106-498."

1502. [Image] The Water Report - Critical habitat, bull trout and politics


	Only portions of issues of The Water Report are available in the Klamath Waters Digital Library. Includes bibliographical references. See the full report at http://www.thewaterreport.com/
	Citation Citation Citation Abstract Copy Title: The Water Report - Critical habitat, bull trout and politics Author: Envirotech Publications Year: 2005, 2008, 2006 Only portions of issues of The Water Report are available in the Klamath Waters Digital Library. Includes bibliographical references. See the full report at http://www.thewaterreport.com/ Title: The Water Report - Critical habitat, bull trout and politics Author: Envirotech Publications Year: 2005, 2008, 2006 Only portions of issues of The Water Report are available in the Klamath Waters Digital Library. Includes bibliographical references. See the full report at http://www.thewaterreport.com/

1503. [Image] The geology and petrography of Crater lake national park


	167, iii p.; xix pl. (incl. 2 maps); Geology by J.S. Diller; Petrography by H.B. Patton; 35.00S
	Citation Citation Citation Abstract Copy Title: The geology and petrography of Crater lake national park Author: Diller, Joseph Silas; Patton, Horace Bushnell Year: 1902, 2006 167, iii p.; xix pl. (incl. 2 maps); Geology by J.S. Diller; Petrography by H.B. Patton; 35.00S Title: The geology and petrography of Crater lake national park Author: Diller, Joseph Silas; Patton, Horace Bushnell Year: 1902, 2006 167, iii p.; xix pl. (incl. 2 maps); Geology by J.S. Diller; Petrography by H.B. Patton; 35.00S

1504. [Image] Klamath River Basin Compact between the states of Oregon and California


	"Ratified by state of Oregon, April 17, 1957 ... and state of California, April 17, 1957 ... consented to by the United States Congress ..."; "[R]epresentative of the United States of America, the States ...
	Citation Citation Citation Abstract Copy Title: Klamath River Basin Compact between the states of Oregon and California Year: 1957, 2004 "Ratified by state of Oregon, April 17, 1957 ... and state of California, April 17, 1957 ... consented to by the United States Congress ..."; "[R]epresentative of the United States of America, the States of California and Oregon have agreed on the compact articles hereinafter set out which were approved by the Klamath River Commissions of Oregon and California on November 17, 1956, and ratified by the Legislatures of Oregon (Chap. 142, Oregon State Laws 1957) and California (Chap. 113, Calif. Statutes 1957) on April 17, 1957. This compact was consented to by Act of Congress (71 Stat. 497) on August 30, 1957, and became effective on September 11, 1957." Title: Klamath River Basin Compact between the states of Oregon and California Year: 1957, 2004 "Ratified by state of Oregon, April 17, 1957 ... and state of California, April 17, 1957 ... consented to by the United States Congress ..."; "[R]epresentative of the United States of America, the States of California and Oregon have agreed on the compact articles hereinafter set out which were approved by the Klamath River Commissions of Oregon and California on November 17, 1956, and ratified by the Legislatures of Oregon (Chap. 142, Oregon State Laws 1957) and California (Chap. 113, Calif. Statutes 1957) on April 17, 1957. This compact was consented to by Act of Congress (71 Stat. 497) on August 30, 1957, and became effective on September 11, 1957."

1505. [Image] Work of the Reclamation service in Washington and Oregon


	The article was written by the Supervising Engineer of the United States Reclamation Service. It includes a photo of the author.
	Citation Citation Citation Abstract Copy Title: Work of the Reclamation service in Washington and Oregon Author: Henny, D.C. Year: 1906, 2005, 2004 The article was written by the Supervising Engineer of the United States Reclamation Service. It includes a photo of the author. Title: Work of the Reclamation service in Washington and Oregon Author: Henny, D.C. Year: 1906, 2005, 2004 The article was written by the Supervising Engineer of the United States Reclamation Service. It includes a photo of the author.

1506. [Image] Integrated land management on Tule Lake Wildlife Refuge: an alternative management strategy developed by the Integrated Land Management Working Group: promoting productive wetland habitats and sustainable agriculture on Tule Lake National Wildlife Refuge


	EXECUTIVE SUMMARY This document describes the rationale for and implementation of an Integrated Land Management (ILM) Plan for the Tule Lake National Wildlife Refuge (NWR). The proposal is the recommendation ...
	Citation Citation Citation Abstract Copy Title: Integrated land management on Tule Lake Wildlife Refuge: an alternative management strategy developed by the Integrated Land Management Working Group: promoting productive wetland habitats and sustainable agriculture on Tule Lake National Wildlife Refuge Author: Integrated Land Management Working Group (Tule Lake National Wildlife Refuge, Calif.) Year: 2000, 2006, 2005 EXECUTIVE SUMMARY This document describes the rationale for and implementation of an Integrated Land Management (ILM) Plan for the Tule Lake National Wildlife Refuge (NWR). The proposal is the recommendation of 5 representative stakeholders in the Tule Lake area. During the 1950fs, 1960fs, and early 1970's, Tule Lake NWR was considered the single most important waterfowl refuge in North America when peak populations exceeded 2.5 million ducks and 1.0 million geese. The Kuchel Act of 1964 was enacted to preserve these waterfowl values as well as the local agricultural economy dependent on Refuge lands. However, restrictive management of wetlands and water levels under the Kuchel Act has eliminated the ecological processes critical to the Refuge's sustained wetland diversity and productivity. Currently, Tule Lake NWR supports a fraction of its past waterfowl use, species diversity has declined, and its value to endangered species has diminished. Agricultural sustainability is also thre Title: Integrated land management on Tule Lake Wildlife Refuge: an alternative management strategy developed by the Integrated Land Management Working Group: promoting productive wetland habitats and sustainable agriculture on Tule Lake National Wildlife Refuge Author: Integrated Land Management Working Group (Tule Lake National Wildlife Refuge, Calif.) Year: 2000, 2006, 2005 EXECUTIVE SUMMARY This document describes the rationale for and implementation of an Integrated Land Management (ILM) Plan for the Tule Lake National Wildlife Refuge (NWR). The proposal is the recommendation of 5 representative stakeholders in the Tule Lake area. During the 1950fs, 1960fs, and early 1970's, Tule Lake NWR was considered the single most important waterfowl refuge in North America when peak populations exceeded 2.5 million ducks and 1.0 million geese. The Kuchel Act of 1964 was enacted to preserve these waterfowl values as well as the local agricultural economy dependent on Refuge lands. However, restrictive management of wetlands and water levels under the Kuchel Act has eliminated the ecological processes critical to the Refuge's sustained wetland diversity and productivity. Currently, Tule Lake NWR supports a fraction of its past waterfowl use, species diversity has declined, and its value to endangered species has diminished. Agricultural sustainability is also thre

1507. [Image] Geothermal Steam Act of 1970 and Regulations on the Leasing of Geothermal Resources


	The Geothermal Steam Act and the implementing Regulations printed here governed most aspects of the leasing of Federal lands for geothermal exploration and development for many years. They are of great ...
	Citation Citation Citation Abstract Copy Title: Geothermal Steam Act of 1970 and Regulations on the Leasing of Geothermal Resources Author: 91st Congress, S.368 Year: 1975 The Geothermal Steam Act and the implementing Regulations printed here governed most aspects of the leasing of Federal lands for geothermal exploration and development for many years. They are of great historical interest. Interesting details include: limits on leased acreage per person or firm, distinctions between competitive and noncompetitive leases, rules for bonus auctions, rents, and production royalties, diligence requirements, and distribution of royalties between the Government and the states. Note that most of what was laid out here prevailed until relatively large revisions in the omnibus Energy Bill of 2005. (DJE 2005) Title: Geothermal Steam Act of 1970 and Regulations on the Leasing of Geothermal Resources Author: 91st Congress, S.368 Year: 1975 The Geothermal Steam Act and the implementing Regulations printed here governed most aspects of the leasing of Federal lands for geothermal exploration and development for many years. They are of great historical interest. Interesting details include: limits on leased acreage per person or firm, distinctions between competitive and noncompetitive leases, rules for bonus auctions, rents, and production royalties, diligence requirements, and distribution of royalties between the Government and the states. Note that most of what was laid out here prevailed until relatively large revisions in the omnibus Energy Bill of 2005. (DJE 2005)

1508. [Image] SFR0028


	Application; Statement of affirmation; Email to Oregon Century Farm and Ranch Program; List of family members; Maps of property; Yamhill County sales data; Copies of photographs; Family history information; ...
	Citation Citation Citation Abstract Copy Title: SFR0028 Author: Oregon Century Farm & Ranch Program; Moberg, Richard; Moberg, Michele (Morris); VanDehey, Cherie (Morris); VanDehey, Mitchell; Fox, Ryan; Fox, Kathy (Morris) Application; Statement of affirmation; Email to Oregon Century Farm and Ranch Program; List of family members; Maps of property; Yamhill County sales data; Copies of photographs; Family history information; Excerpt from "History of Oregon"; Newspaper articles; Farm history narrative; Original century farm application; Excerpt from "Genealogical Material in Oregon Donation Land Claims, Volume 1"; Map of property; Copy of original Donation Land Claim certificates; Architectural drawings; Index card for Historic American Buildings Survey; Photographs; Plat map.; 2014 Title: SFR0028 Author: Oregon Century Farm & Ranch Program; Moberg, Richard; Moberg, Michele (Morris); VanDehey, Cherie (Morris); VanDehey, Mitchell; Fox, Ryan; Fox, Kathy (Morris) Application; Statement of affirmation; Email to Oregon Century Farm and Ranch Program; List of family members; Maps of property; Yamhill County sales data; Copies of photographs; Family history information; Excerpt from "History of Oregon"; Newspaper articles; Farm history narrative; Original century farm application; Excerpt from "Genealogical Material in Oregon Donation Land Claims, Volume 1"; Map of property; Copy of original Donation Land Claim certificates; Architectural drawings; Index card for Historic American Buildings Survey; Photographs; Plat map.; 2014

1509. [Image] Integrated scientific assessment for ecosystem management in the interior Columbia Basin and portions of the Klamath and Great Basins


	Abstract Quigley, Thomas M.; Haynes, Richard W.; Graham, Russell T., tech. eds. 1996. Integrated scientific assessment for ecosystem management in the interior Columbia basin and portions of the Klamath ...
	Citation Citation Citation Abstract Copy Title: Integrated scientific assessment for ecosystem management in the interior Columbia Basin and portions of the Klamath and Great Basins Year: 1996, 2005, 2000 Abstract Quigley, Thomas M.; Haynes, Richard W.; Graham, Russell T., tech. eds. 1996. Integrated scientific assessment for ecosystem management in the interior Columbia basin and portions of the Klamath and Great Basins. Gen. Tech. Rep. PNW-GTR-382. Portland, OR: U.S. Department of Agriculture, Forest Service, Pacific Northwest Research Station. 303 p. (Quigley, Thomas M., tech. ed. The Interior Columbia Basin Ecosystem Management Project: Scientific Assessment.) The Integrated Scientific Assessment for Ecosystem Management for the Interior Columbia Basin links landscape, aquatic, terrestrial, social, and economic characterizations to describe biophysical and social systems. Integration was achieved through a framework built around six goals for ecosystem management and three different views of the future. These goals are: maintain evolutionary and ecological processes; manage for multiple ecological domains and evolutionary timeframes; maintain viable populations of native and desired non-native species; encourage social and economic resiliency; manage for places with definable values; and, manage to maintain a variety of ecosystem goods, services, and conditions that society wants. Ratings of relative ecological integrity and socioeconomic resiliency were used to make broad statements about ecosystem conditions in the Basin. Currently in the Basin high integrity and resiliency are found on 16 and 20 percent of the area, respectively. Low integrity and resiliency are found on 60 and 68 percent of the area. Different approaches to management can alter the risks to the assets of people living in the Basin and to the ecosystem itself. Continuation of current management leads to increasing risks while management approaches focusing on reserves or restoration result in trends that mostly stabilize or reduce risks. Even where ecological integrity is projected to improve with the application of active management, population increases and the pressures of expanding demands on resources may cause increasing trends in risk. Keywords: Ecosystem assessment, management and goals; ecological integrity; socio-economic resiliency; risk management Title: Integrated scientific assessment for ecosystem management in the interior Columbia Basin and portions of the Klamath and Great Basins Year: 1996, 2005, 2000 Abstract Quigley, Thomas M.; Haynes, Richard W.; Graham, Russell T., tech. eds. 1996. Integrated scientific assessment for ecosystem management in the interior Columbia basin and portions of the Klamath and Great Basins. Gen. Tech. Rep. PNW-GTR-382. Portland, OR: U.S. Department of Agriculture, Forest Service, Pacific Northwest Research Station. 303 p. (Quigley, Thomas M., tech. ed. The Interior Columbia Basin Ecosystem Management Project: Scientific Assessment.) The Integrated Scientific Assessment for Ecosystem Management for the Interior Columbia Basin links landscape, aquatic, terrestrial, social, and economic characterizations to describe biophysical and social systems. Integration was achieved through a framework built around six goals for ecosystem management and three different views of the future. These goals are: maintain evolutionary and ecological processes; manage for multiple ecological domains and evolutionary timeframes; maintain viable populations of native and desired non-native species; encourage social and economic resiliency; manage for places with definable values; and, manage to maintain a variety of ecosystem goods, services, and conditions that society wants. Ratings of relative ecological integrity and socioeconomic resiliency were used to make broad statements about ecosystem conditions in the Basin. Currently in the Basin high integrity and resiliency are found on 16 and 20 percent of the area, respectively. Low integrity and resiliency are found on 60 and 68 percent of the area. Different approaches to management can alter the risks to the assets of people living in the Basin and to the ecosystem itself. Continuation of current management leads to increasing risks while management approaches focusing on reserves or restoration result in trends that mostly stabilize or reduce risks. Even where ecological integrity is projected to improve with the application of active management, population increases and the pressures of expanding demands on resources may cause increasing trends in risk. Keywords: Ecosystem assessment, management and goals; ecological integrity; socio-economic resiliency; risk management

1510. [Image] Recent paleolimnology of Upper Klamath Lake, Oregon


	Recent Paleolimnology of Upper Klamath Lake Eilers et al. 2001 ABSTRACT Sediment cores were collected from Upper Klamath Lake in October, 1998 and analyzed for 210Pb, 14C, 15N, N, P, C, Ti, Al, diatoms, ...
	Citation Citation Citation Abstract Copy Title: Recent paleolimnology of Upper Klamath Lake, Oregon Author: United States. Bureau of Reclamation Year: 2001, 2005 Recent Paleolimnology of Upper Klamath Lake Eilers et al. 2001 ABSTRACT Sediment cores were collected from Upper Klamath Lake in October, 1998 and analyzed for 210Pb, 14C, 15N, N, P, C, Ti, Al, diatoms, Pediastrum, and cyanobacterial akinetes. These results were used to reconstruct changes in water quality in Upper Klamath Lake over the last 150 years. The results showed that there was substantial mixing of the upper 10 cm of sediment, representing the previous 20 to 30 years. However, below that, 210Pb activity declined monotonically, allowing reasonable dating for the period from about 1850 to 1970. The sediment accumulation rates (SAR) showed a substantial increase in the 20th century. The increase in SAR corresponded with increases in erosional input from the watershed as represented by the increases in sediment concentrations of Ti and Al. The upper 20 cm of sediment (representing the last 150 years) also showed increases in C, N, P, and 15N. The increases in nutrient concentrations may be affected to various degrees by diagenetic reactions within the sediments, although the changes in concentrations also were marked by changes in the N:P ratio and in a qualitative change in the source of N as reflected in increasing S15N. The diatoms showed modest changes, particularly in the upper sediments, with increases in Asterionellaformosa, Stephanodiscus hantzschii, and S. parvus. Pediastrum, a green alga, was well-preserved in the sediments and exhibited a sharp decline in relative abundance in the upper sediments. Total cyanobacteria, as represented by preserved akinetes, exhibited only minor changes in the last 1000 years. However, a taxon which was formerly not present in the lake 150 years ago, Aphanizomenon, has shown major increases in recent decades. Although the mixing in the upper sediments prevents high-resolution temporal analysis of the recent history (e.g. last 30 years) of Upper Klamath Lake, the results demonstrate that major changes in water quality likely have occurred leading to a major modification of the phytoplankton assemblage. The changes in sediment composition are consistent with land use activities during this period that include substantial deforestation, drainage of wetlands, and agricultural activities associated with livestock and irrigated cropland. Title: Recent paleolimnology of Upper Klamath Lake, Oregon Author: United States. Bureau of Reclamation Year: 2001, 2005 Recent Paleolimnology of Upper Klamath Lake Eilers et al. 2001 ABSTRACT Sediment cores were collected from Upper Klamath Lake in October, 1998 and analyzed for 210Pb, 14C, 15N, N, P, C, Ti, Al, diatoms, Pediastrum, and cyanobacterial akinetes. These results were used to reconstruct changes in water quality in Upper Klamath Lake over the last 150 years. The results showed that there was substantial mixing of the upper 10 cm of sediment, representing the previous 20 to 30 years. However, below that, 210Pb activity declined monotonically, allowing reasonable dating for the period from about 1850 to 1970. The sediment accumulation rates (SAR) showed a substantial increase in the 20th century. The increase in SAR corresponded with increases in erosional input from the watershed as represented by the increases in sediment concentrations of Ti and Al. The upper 20 cm of sediment (representing the last 150 years) also showed increases in C, N, P, and 15N. The increases in nutrient concentrations may be affected to various degrees by diagenetic reactions within the sediments, although the changes in concentrations also were marked by changes in the N:P ratio and in a qualitative change in the source of N as reflected in increasing S15N. The diatoms showed modest changes, particularly in the upper sediments, with increases in Asterionellaformosa, Stephanodiscus hantzschii, and S. parvus. Pediastrum, a green alga, was well-preserved in the sediments and exhibited a sharp decline in relative abundance in the upper sediments. Total cyanobacteria, as represented by preserved akinetes, exhibited only minor changes in the last 1000 years. However, a taxon which was formerly not present in the lake 150 years ago, Aphanizomenon, has shown major increases in recent decades. Although the mixing in the upper sediments prevents high-resolution temporal analysis of the recent history (e.g. last 30 years) of Upper Klamath Lake, the results demonstrate that major changes in water quality likely have occurred leading to a major modification of the phytoplankton assemblage. The changes in sediment composition are consistent with land use activities during this period that include substantial deforestation, drainage of wetlands, and agricultural activities associated with livestock and irrigated cropland.

1511. [Image] Seeking refuge: making space for migratory waterfowl and wetlands along the Pacific Flyway


	Abstract "Seeking Refuge" examines the history of migratory waterfowl management along the Pacific Flyway, the westernmost of four main migration routes in North America. Drawing on approaches from historical ...
	Citation Citation Citation Abstract Copy Title: Seeking refuge: making space for migratory waterfowl and wetlands along the Pacific Flyway Author: Wilson, Robert Michael Year: 2003, 2005, 2004 Abstract "Seeking Refuge" examines the history of migratory waterfowl management along the Pacific Flyway, the westernmost of four main migration routes in North America. Drawing on approaches from historical geography and environmental history, this study shows how wildlife officials developed migratory bird refuges in Oregon and California, where over 60 percent of Pacific Flyway waterfowl winter. During the early-twentieth century, reclamation and river diking eliminated most of the wetlands in the birds' wintering range. Bird enthusiasts such as bird watchers and duck hunters successfully lobbied for the creation of wildlife refuges in a few areas along the flyway. These early refuges failed to protect waterfowl habitat and they were severely degraded by reclamation. In the 1930s and 1940s, the U.S. Fish and Wildlife Service (FWS) and its predecessor, the Bureau of Biological Survey, undertook an ambitious program to resurrect these sanctuaries and to create new ones. Many farmers opposed these refuges out of fear that waterfowl would damage crops. To respond to these concerns and to ensure an adequate food supply for the birds, the FWS raised rice, barley, and other grains. The agency adopted many of the technologies of modern, industrial agriculture including synthetic herbicides and insecticides such as 2, 4-D and DDT. By the 1960s, the refuges had become largely mirrors of the surrounding irrigated farmlands, the main difference being that the FWS raised grain for waterfowl rather than for market. Refuges could not escape the agricultural settings in which they were embedded. As units within the irrigated countryside, Pacific Flyway refuges were often at the mercy of nearby farmers and federal reclamation agencies. Poor water quality and insufficient supplies of water often hampered FWS efforts to manage refuges. In the late-twentieth century, reduced water supply due to diversions to California municipalities and to sustain endangered fish species affected the amount of water reaching refuges. This dissertation has other goals. First, it critiques the anthropocentrism of most historical geography by focusing on how political, cultural, and ecological factors affected wildlife. Second, it contributes to the literature on the state's role in environmental protection by investigating the overlapping, and often contradictory, spaces within which wildlife managers implemented environmental regulations. Title: Seeking refuge: making space for migratory waterfowl and wetlands along the Pacific Flyway Author: Wilson, Robert Michael Year: 2003, 2005, 2004 Abstract "Seeking Refuge" examines the history of migratory waterfowl management along the Pacific Flyway, the westernmost of four main migration routes in North America. Drawing on approaches from historical geography and environmental history, this study shows how wildlife officials developed migratory bird refuges in Oregon and California, where over 60 percent of Pacific Flyway waterfowl winter. During the early-twentieth century, reclamation and river diking eliminated most of the wetlands in the birds' wintering range. Bird enthusiasts such as bird watchers and duck hunters successfully lobbied for the creation of wildlife refuges in a few areas along the flyway. These early refuges failed to protect waterfowl habitat and they were severely degraded by reclamation. In the 1930s and 1940s, the U.S. Fish and Wildlife Service (FWS) and its predecessor, the Bureau of Biological Survey, undertook an ambitious program to resurrect these sanctuaries and to create new ones. Many farmers opposed these refuges out of fear that waterfowl would damage crops. To respond to these concerns and to ensure an adequate food supply for the birds, the FWS raised rice, barley, and other grains. The agency adopted many of the technologies of modern, industrial agriculture including synthetic herbicides and insecticides such as 2, 4-D and DDT. By the 1960s, the refuges had become largely mirrors of the surrounding irrigated farmlands, the main difference being that the FWS raised grain for waterfowl rather than for market. Refuges could not escape the agricultural settings in which they were embedded. As units within the irrigated countryside, Pacific Flyway refuges were often at the mercy of nearby farmers and federal reclamation agencies. Poor water quality and insufficient supplies of water often hampered FWS efforts to manage refuges. In the late-twentieth century, reduced water supply due to diversions to California municipalities and to sustain endangered fish species affected the amount of water reaching refuges. This dissertation has other goals. First, it critiques the anthropocentrism of most historical geography by focusing on how political, cultural, and ecological factors affected wildlife. Second, it contributes to the literature on the state's role in environmental protection by investigating the overlapping, and often contradictory, spaces within which wildlife managers implemented environmental regulations.

1512. [Image] Lakeview proposed resource management plan and final environmental impact statement [volume 1]


	4 v.; maps (some col.); "August 2002"; "January 2003" -- cover
	Citation Citation Citation Abstract Copy Title: Lakeview proposed resource management plan and final environmental impact statement [volume 1] Author: U.S. Department of the Interior. Bureau of Land Management; Lakeview Resource Area Office. Lakeview District Year: 2002, 2006, 2005 4 v.; maps (some col.); "August 2002"; "January 2003" -- cover Title: Lakeview proposed resource management plan and final environmental impact statement [volume 1] Author: U.S. Department of the Interior. Bureau of Land Management; Lakeview Resource Area Office. Lakeview District Year: 2002, 2006, 2005 4 v.; maps (some col.); "August 2002"; "January 2003" -- cover

1513. [Image] The South Portal Project : creating a sense of arrival


	"Holistic planning for Lake Ewauna & the south entry to the City of Klamath Falls"
	Citation Citation Citation Abstract Copy Title: The South Portal Project : creating a sense of arrival Author: Carpenter Design, Inc. Year: 2005 "Holistic planning for Lake Ewauna & the south entry to the City of Klamath Falls" Title: The South Portal Project : creating a sense of arrival Author: Carpenter Design, Inc. Year: 2005 "Holistic planning for Lake Ewauna & the south entry to the City of Klamath Falls"

1514. [Image] Klamath Falls Resource Area resource management plan and environmental impact statement : final : Volume 1


	Proposed resource management plan/final environmental impact statement for the Klamath Falls Resource Area
	Citation Citation Citation Abstract Copy Title: Klamath Falls Resource Area resource management plan and environmental impact statement : final : Volume 1 Author: United States. Bureau of Land Management. Klamath Falls Resource Area Office Year: 1994, 2005, 2004 Proposed resource management plan/final environmental impact statement for the Klamath Falls Resource Area Title: Klamath Falls Resource Area resource management plan and environmental impact statement : final : Volume 1 Author: United States. Bureau of Land Management. Klamath Falls Resource Area Office Year: 1994, 2005, 2004 Proposed resource management plan/final environmental impact statement for the Klamath Falls Resource Area

1515. [Image] Evaluation of site specific restoration projects for the entire Klamath River basin


	DOCS I 49.107: 89 ( 1.1) 89( 1.1) EVALUATION OF SITE SPECIFIC RESTORATION PROJECTS FOR THE ENTIRE KLAMATH RIVER BASIN. 1989 Klamath Field Review Comments The following comments are based primarily upon ...
	Citation Citation Citation Abstract Copy Title: Evaluation of site specific restoration projects for the entire Klamath River basin Year: 1989, 2005 DOCS I 49.107: 89 ( 1.1) 89( 1.1) EVALUATION OF SITE SPECIFIC RESTORATION PROJECTS FOR THE ENTIRE KLAMATH RIVER BASIN. 1989 Klamath Field Review Comments The following comments are based primarily upon field observations made by Scott Downie and Andy Kier during the summer and autumn of 1989, Some of the review was made accompanied by personnel responsible for the projects and their comments are incorporated as well. In many streams individual project sites are linked and/ or similar in nature. This review generalizes these in its comments and ratings, but notes exceptions where required. Grades A- F were assigned, but like all grades lacking set criteria and good base- line information, they are somewhat subjective. Evaluations were based upon the observed or perceived physical response mf. de by the stream to the project, whether or not the project satisfied the objectives of the proposal, and whether or not the project appeared to have durable structure and function without maintenance or modification. Biological evaluation was impossible except to note observed fish at the time of the review. Cost effectiveness is again somewhat subjective without more front- end information, but based upon personal experience an attempt to measure product for cost entered into grade assignment. GENERAL: 1000, 1001, 1003: The racks on Bogus Crk, Scott R. & Shasta R were all operational Summer 1989. 1002: The Salmon R. weir operations were modified during our review period in response to public input: 1. The trap and weir will be staffed 24 hrs/ day. 2. Weir and trap operations will cease at 73 F. 3. Fishing will not be allowed below weir. 4. An alternate site will be developed ASAP. LOWER KLAMATH SUBBASIN: Ah Pah Creek ( 11006, 07, 08, 09, 10, 18-$ 123,928): A CCC, DFG, & Simpson Timber Co. project to provide improved access for adults into upper Ah Pah Crk., and to control sedimentation from failing banks in the treatment area. In Oct. 1989, the Hewitt Ramp structures were successfully passing coho and steelhead adults and juveni'es through a previous adult barrier section. Large wood and boulder cover elements had been placed in the associated pools. Treated banks were armored with rock filled gabions and planted with alder, willow and conifers. No evidence of sediment production to the stream from these treated slopes was observed. The workmanship and construction are sturdyand of high quality. Grade A. { Since we visited Ah Pah Crk. the day after the RNP bypass failure, the stream was loaded with suspended sediments) 1990 - Review Comments- Bluff Creek ( 11022, 23, 24, 31, 32-$ 212,000): Access provided through lower Bluff Crk's former barrier section is still passing adults and juveniles following the Feb. 1986 flood event. The boulder weirs and boulder clusters near the yearling rearing facility are providing limited spawning improvement, but they do contain pockets of gravel utilized by spawners. Both the weirs and clusters have provided some good quality summer rearing habitats, and also refuge areas during winter flows. Two cluster groups are now buried under large streambank failures. These events could have been exacerbated by the placement of the boulders too close to the now failed right bank. No large wood or brush cover elements were utilized in the structures, although some were available. Personnel explained that the extreme velocities and power at high discharges prevented incorporating these organic components into their instream structures on Bluff Crk, Grade C. Camp Creek ( 11029, 30-$ 125,000): Six boulder weirs were constructed by USFS to trap spawning gravels. Two of the six weirs are now scattered boulder clusters, having been rearranged by the stream. The surviving weirs have provided gravels and are being used by fish. The boulder groups, both designed and incidental, are providing some good quality rearing habitats and some pockets of gravel used for spawning salmonids. 3rade C. Cappell Creek ( 11027-$ 125,000): BIA artificial propagation project. Project has operated for one year. It has released 17,035 CWT Chinook. Typical of the lower river hatchery programs, securing desired numbers of late running chinook broodstocks is very difficult. A lot of money in terms of fry produced, but the facility start- up costs are now over and the annual cost will be much less than the initial investment. Grade C. Hunter Creek ( 11001, 11002, 11013-$ 19,328): A CCC, DFG, and Simpson project to improve Hunter Creek on a basin scale. CCC now have a thorough instream assessment and instream structure plan prepared by Clearwater Biostudies, inc. under contract to them. Instream structure work is now underway by CCC crews. The construction is of excellent quality and design. All upper stream barrier work is now completed. The dry lower reaches of the stream pose a dewatered, complete barrier to all adults running before early November in most years ( T. Payne, 1989). Some concern over future land management's effect on the stream in the event of a major flood occurrence. Grade B. McGarvey Creek ( 11025, 11014, 11003-$ 24,264): Status of the hatch box project is not known. The barrier work is all done and passing fish. Grade C. - Review Comments- Pecwan Creek ( 11021, 11036, 11028-$ 50,000): A total of 21,626 yearling chinook were released from 1982- 84 from this facility* They were from Iron Gate stocks and deemed not suitable for the restocking goals of the project area. Since 1985, the facility's production is not well documented, but 27,000 for the period 1985- 88 is estimated. None of the releases from this site have been CWT. The Pecwan site has been used as a broodstock source for Cappell Creek as well. Grade D. Red Cap Creek ( 11033, 34, 35-$ 70,000): USFS project has produced some impressive results. Failing banks have been armored and vegetated. A series of over thirty boulder weirs and clusters have provided some high quality spawning and rearing habitats. Large wood cover elements have been used somewhat in the project. The project reach is in a stream section of former generally poor habitats and low utilization by salmonids; they were abundant during our visits. There is a yearling pond adjacent to the treatment section. Grade A. Richardson Creek ( 11026-$ 25,200): This project removed a barrier to salmonids and is functional. Seemed expensive. Grade C. Salt Creek ( 11000, 11012-$ 18,944): CCC successfully stabilized failing banks. All barrier work is completed and functional. One of the few upslope erosion control projects in the review has controlled the sediment output from the roadway. There is a lot of product here for the money. Grade A. Surpur Creek ( 11005-$ 3,456): CCC removed barriers at a bargain price. Still functional. Grade A. Tarup Creek ( 11004, 11011, 11015, 16, 17-$ 77,024): CCC has a plan for the creek and instream treatments done under contract by Inter- Fluv Inc. The work outlined in the plan is now completed, and is of very high quality and design for the most part. The work involved barrier modification, instream structures, revegetation upslope as well in the riparian zone, and some upslope erosion control ( one site upslope was quite major, in fact). Tarup, regardless of all these improvements, has a low flow access problem in its delta. Grade B. Pine Creek ( 10019, 20-$- 0-): Not reviewed. Various streams ( 11019- 20-$ 550,000): This is the CCC operation fund for the Lower Klamath program. This ongoing general fund was not deemed suitable for field review or rating. However, our general observation of the CCC/ DFG Lower Klamath program has certainly produced a positive impression of their work and approach. - Review Comments- MIDDLE KLAMATH SUBBASIN: Beaver Creek ( 6000- 05, 6035, 6053, 6065, 6066-$ 124,400): The boulder cluster groups and weirs constructed on Beaver Creek are not well utilized at this time. Silts and sediments nave impacted the quality of the gravel associated with the structures to the extent that some cementing has occurred. Therefore, it is believed that utilization by spawners has also been effected. The structures designed for the provision of rearing habitats have done better, and some of course do both, some neither. Grade C, The rearing facility ( 6035) was closed in 1985, but there is now talk of re- opening it. 1980- 84 releases averaged 29,423 yearling chinook of Iron Gate origin. Grade C. The gravel seeding occurred in 1985 ( 6052) and no evaluation was considered possible in 1989, nor was any proffered by staff. The two screens ( 6065- 66) are functional, but require regular upkeep and periodic thorough maintenance. Grade B. Bluff Creek ( 6036-$- 0-): This is one of the Klamath system's highest production cooperative rearing facilities. It has averaged 66,462 chinook yearlings for the past three years. These fish are of Iron Gate origin. Although adult runs are up in Bluff Creek, there is little baseline data, and until the current brood no CWT's were done on the ponded fish. Grade B. Bogus Creek ( 6046- 47, 6053- 54, 6061-$ 94,750): Bogus Creek is heavily utilized by naturally spawning chinook of Iron Gate Hatchery origin as well as by stocks of its own. The projects designed to provide more and/ or better gravels for these fish have met with apparent success, since in almost all cases the projects are used by the spawners, but so is everything else. What that means in real incremental gains that can be credited to particular habitat treatments is therefore difficult to assess. CWT and DSM evaluation programs are ongoing. Grade C. Camp Creek ( 6037-$- 0-): This rearing facility switched from Iron Gate chinook stocks to natal stocks in 1987. Yearling releases dropped from an average of 27,533 to 14,573 after the change. This can be attributed to the difficulty in trapping adults in an open, high discharge system. Still, the fact that they are now utilizing later running stocks that are adapted to Camp Creek's flow regime and conditions counts for a great deal. The natal brood have been marked with alternating maxillary clips ( right one year, left the next) prior to release and some have been recovered as adults. Grade B+. China Creek ( 6008- 09-$ 9,300): Not reviewed. Report is that the access is good throughout the stream now. No report on the status of the structures. - Review Comments- Clear Creek ( 6010, 6068- 69-$ 66,400): Fish and Game's barrier removal is providing access successfully. Report is that access is good throughout Clear Creek at this time. Grade B. Coon Creek ( 6056-$ 30,000): This ladder passes steelhead, but DFG is not certain about coho. It also requires some light upkeep. Grade B. Cottonwood Creek ( 6049-$ 22,966): Gravel placed on these weirs needs to be re- seeded periodically at the cost of $ 2,000 each time. Grade D. ( 6057-$ 6,000): Not reviewed. ( 6055-$ 5,000): Ladder is on line and working well. Grade B. ( 6058- 60-$ 29,500): These screens are all on line and operational, but require light periodic maintenance which is conducted by the Yreka Screen Shop on a rotating basis. Grade B. ( 6070-$ 1,200): The potholes blasted to trap gravel have trapped sand instead, so the goal of creating spawning habitat was not met. However, fry usage and survival seem to be good in the resultant pools. Not a high cost project. Grade C. ( Total Cottonwood Creek budget: $ 64,666) Di1lon Creek ( 6071-$ 5,000): This functional project opened five miles of good habitat now utilized by steelhead and Chinook. Grade A. Doolittle Creek ( 6011-$ 2,300) : The treated log jam has not reformed and access is still good for steelhead. Grade C. Elk Creek ( 6012- 14-$ 41,000): The boulder weirs and clusters are now all installed and need flows for evaluation of performance. ( 6034, 6045-$ 10,000) : The washout pond has averaged 31,205 released Iron Gate chinook yearlings since 1984. Grade B. ( Total Elk Creek budget: $ 51,000) Grider Creek ( 6015- 16, 6038-$ 18,500): The falls are now passing fish successfully. Grade A. The boulder weirs have been successful in trapping spawning gravel and are being used by chinook. Grade A. The ponds have grown an average of 34,426 Iron Gate chinook yearlings since 1987. Grade B. Horse Creek ( 6062- 64, 6074-$ 35,000): The three screens are installed and operational, but require light maintenance. Yreka Screen Shop provides this on an alternating basis. Grade B. The log jam is no longer an access problem. Grade A. ( Extant diversion dam is a major problem on this creek) Humbug Creek ( 6017- 18-$ 5,300): The boulder weirs are not successful and are physically failing. Grade F. The log weirs have worked well and are providing spawning and rearing habitat. Grade A. In any event, ten miles of good quality habitat are blocked to salmonids by dredge tailings in lower Humbug Creek. - Review Comments- Independence Creek ( 6019-$ 5,000): The stream's mouth is still open and fish access it. Grade B. Indian Creek ( 6006, 6020- 28, 6039- 40, 6067, 6072~$ 200,600): AH modified former barriers are now passing fish. Grade A. The recent instream structures all appear to be performing to design; biological evaluation is underway now. Grade B. The spawning channel is used extensively by steelhead, and to a lesser extent by coho, but not by chinook. It is also a maintenance item ( ie. supplemental gravel). Grade D. The rearing ponds have averaged 74,134 Iron Gate yearlings since 1985. Grade B. Irving Creek ( 6029-$ 9,300): The use of small boulders to construct inadequately sized structures resulted in no net gain from this project. Grade F. Iron Gate Hatchery ( 6033-$-?-): The hatchery is modifying its operations to better cope with problems associated with temperatures, density, and release timing according to the hatchery manager. Grade C. Badger Flat and Tree of Heaven ( 6050- 51-$ 136,000): These spawning channels have both been unsuccessful due to design flaws. They require constant maintenance which is not possible during usage. Gravel seeding is an ongoing project. Grade F. Little Bogus Creek ( 6048-$ 20,000): These seeded weirs were not reviewed, but they are reported to be intensely utilized by spawners. However, some maintenance is also required. Pearch Creek ( 6041-$- 0-): These ponds are operated by the Orleans Rod and Gun Club and have good public involvement and educational value. About 9,000 steelhead of Salmon River origin are reared here. A lot of enthusiasm and local stocks. Grade A. Red Cap Creek ( 6042-$- 0-): This rearing pond has averaged 37,862 Iron Gate chinook yearlings since 1985 and is operated in a system that has also had significant habitat improvement projects recently completed. A CWT program would help evaluate both of these aspects of the Red Cap Creek endeavor. Grade B. Seiad Creek ( 6030- 31, 6073-$ 5,100): The barrier project has been successful. Grade A. The weir projects were not found and therefore not reviewed. Thompson Creek ( 6032, 6043-$ 5,000): The rearing ponds were closed in 1985. The instream structures were not reviewed. West Branch Creek ( 6007-$ 5,500): The weirs are used by steelhead for spawning, according to local observers; they seem functional. Grade C. - Review Comments- Wilson Creek ( 6007-$- 0-): This private rearing facility was not reviewed. According to locals, it is not in use at this time. SALMON RIVER: Black Bear Creek ( 5000-$ 11,000): This USFS project successfully provided access for steelhead into the creek, and it is currently being utilized. Grade A. Kelly Gulch ( 5002- 03-$ 9,500): This project was not reviewed, but USFS staff reported that the barrier was still not passing all fish attempting to access the system. Their evaluation is underway now. Knownothing Creek ( 5004- 06, 5021-$ 153,114): The removal of the diversion dams and other barriers resulted, in doubling the chinook and coho runs into the creek. Grade A. The weirs ( 5006) were not completed at the time of the review. Delays were incurred because the rock was overshot resulting in boulders too small for the structures. Grade F. Nordheimer Creek ( 5007, 5008-$ 90,000): The log weirs ( 5007) failed. Grade F. The fishway ( 5008) is successful and passing fish. Grade A. Salmon River ( 5023, 5024-$ 8,000): This selective barrier was modified at a very reasonable cost and has improved access for al1 fish. Grade A. East Fork Salmon River ( 5013-$ 60,000): This project was not reviewed; USFS is evaluating now. South Fork Salmon River ( 5009- 12, 5014- 15, 5022, 5001-$ 176,200): ( 5009) This natal stock bioenhancement facility was located at a site with poor water temperature conditions for intense fish culture. Broodstock acquisition was also very difficult. The facility is now closed ( equipment will be relocated in the watershed, if possible). The project released 36,667 natal chinook smolts in the period from 1985 to 1987. Grade D. The boulder group projects were undergoing evaluation during the review period for biological response. The initial physical evaluation was not conclusive because many of the projects had not been subject to higher flows. Grade C. ( 5022) The " rough passage" area currently allows fish to pass without undue struggle. Grade B. ( 5001) The Blind Horse Creek weirs have not all been successful in providing spawning habitat. Many are trapping silt rather than spawning gravel. Rearing habitats are being provided by most of them, however. Grade D. - Review Comments- Specimen Creek ( 5016-$ 500): Steelhead now pass the treated log jam barrier. Another jam has formed above this site and requires monitoring and possible modification. Grade B. St. Claire Creek ( 5017- 20-$ 15,000): Steelhead now pass the modified barrier. The log weirs are holding gravel and in use by spawners. Juvenile cover is good associated with the weirs as well as the cover elements used in the project. The boulder weirs and clusters are also in place and in use. Grade A. SCOTT RIVER: Scott River and tribs. ( 4031- 4334 [ not inclusive]-$ 2, " 15,810) : These Soil Conservation District projects primarily involved placing rip- rap armor at 304 different sites in the upper Scott system. Not all were reviewed, and although the rock is stable and in place, many were found to lack streamside vegetation that would provide important shade and cover for the stream and aquatic life. Some others were buried in decomposed granite, sand or silt and therefore had little benefit for fish by way of providing complex micro- habitats. The value of these projects would be much greater if some of these items were addressed. Grade C. French Creek ( 4001, 4016- 18-$ 32,100): The sediment check dam initially filled in one storm event. It was excavated but refilled during the next runoff event. A high maintenance approach that treats the symptoms of the watershed's chronic erosion problem. Grade F. The screens are all in place and functional, but are dependent upon periodic light upkeep provided by the Yreka Screen Shop. Grade B. Kelsey Creek ( 4002- 04-$ 147,500): The weirs work well and are used by all species for spawning and rearing. Grade A. The USFS spawning channel has not performed as hoped. Problems have occurred relating to channel liner failure. The average number of pairs using the channel during the period 1985- 88 were: nine chinook, three coho, and twelve steelhead. In 1989 no usage was observed. It is also a very costly installation. Grade D-. Kidder Creek ( 4020- 21-$ 26,000): Both screens are in place and functional, but are dependent upon periodic maintenance provided by the Yreka Screen Shop. Grade B. Patterson Creek ( 4019-$ 9,000): This screen is in place and functional, but is dependent upon periodic maintenance provided by the Yreka Screen Shop. Grade B. - Review Comments- Scott River ( 4005- 06, 4012- 15-$ 94,800): Although the gravels were ' cleaned' the sedimentation problem returned the next year, This treatment does not address the problem, but rather the symptoms and would require constant maintenance. Grade F. The boulder groups were not installed after gauging the rapid sedimentation rate. The four screens are in place and functional, but are dependent upon periodic maintenance provided by the Yreka Screen Shop. Grade B. East Fork Scott River ( 4010- 11-$ 20,000): These two screens are in place and functional, but are dependent upon periodic maintenance provided by the Yreka Screen Shop. Grade B. Shakleford Creek ( 4009, 4022- 4030 incl., 4323, 4329-$ 343,720): ( 4009) The bank armor was not surveyed, but is reported to be stabilizing the soft banks. The fishery benefits are not known, ( 4022- 30) These nine screens are in place and functional, but are dependent upon periodic maintenance provided by tne Yreka Screen Shop, Grade B. ( 4323, 4329) The rip- rap bank armor is in place, but needs vegetation and cover elements added to increase fishery values. Grade C. Thomkins Creek ( 4007- 08-$ 6,500): The weirs are installed but are not highly utilized because of the recruited fine sediments now accumulated on them. Grade D. The fishway has provided access and is currently functional. Grade B. SHASTA RIVER: Parks Creek ( 3018-$ 42,000): These four screens are in place and functional, but are dependent upon periodic maintenance provided by the Yreka Screen Shop. Grade B. Shasta River ( 3000- 04, 3005- 08, 3009- 17-$ 519,000): ( 3000- 04) These weirs have deteriorated over the past few years due to the use of undersized boulders in construction. Only about 10% of the effective structures remain. In 1989 only 32 redds were observed on the weirs. Very expensive ($ 363,000) spawning gravel. Grade D. The four fishways ( 3005- 08-$ 17,000) are all currently passing fish. Grade B. The nine screens ( 3009- 17-$ 139,000) are in place and functional, but are dependent upon periodic maintenance provided by the Yreka Screen Shop. Grade B. 12 0140402500 UPPER KLAMATH RIVER: Fal1 Creek ( 2000-$- 0-): The Fall Creek hatchery facility is on line and ready to augment Iron Gate's production. The site has very good water quality and can be instrumental in relieving crowding problems at Iron Gate. Title: Evaluation of site specific restoration projects for the entire Klamath River basin Year: 1989, 2005 DOCS I 49.107: 89 ( 1.1) 89( 1.1) EVALUATION OF SITE SPECIFIC RESTORATION PROJECTS FOR THE ENTIRE KLAMATH RIVER BASIN. 1989 Klamath Field Review Comments The following comments are based primarily upon field observations made by Scott Downie and Andy Kier during the summer and autumn of 1989, Some of the review was made accompanied by personnel responsible for the projects and their comments are incorporated as well. In many streams individual project sites are linked and/ or similar in nature. This review generalizes these in its comments and ratings, but notes exceptions where required. Grades A- F were assigned, but like all grades lacking set criteria and good base- line information, they are somewhat subjective. Evaluations were based upon the observed or perceived physical response mf. de by the stream to the project, whether or not the project satisfied the objectives of the proposal, and whether or not the project appeared to have durable structure and function without maintenance or modification. Biological evaluation was impossible except to note observed fish at the time of the review. Cost effectiveness is again somewhat subjective without more front- end information, but based upon personal experience an attempt to measure product for cost entered into grade assignment. GENERAL: 1000, 1001, 1003: The racks on Bogus Crk, Scott R. & Shasta R were all operational Summer 1989. 1002: The Salmon R. weir operations were modified during our review period in response to public input: 1. The trap and weir will be staffed 24 hrs/ day. 2. Weir and trap operations will cease at 73 F. 3. Fishing will not be allowed below weir. 4. An alternate site will be developed ASAP. LOWER KLAMATH SUBBASIN: Ah Pah Creek ( 11006, 07, 08, 09, 10, 18-$ 123,928): A CCC, DFG, & Simpson Timber Co. project to provide improved access for adults into upper Ah Pah Crk., and to control sedimentation from failing banks in the treatment area. In Oct. 1989, the Hewitt Ramp structures were successfully passing coho and steelhead adults and juveni'es through a previous adult barrier section. Large wood and boulder cover elements had been placed in the associated pools. Treated banks were armored with rock filled gabions and planted with alder, willow and conifers. No evidence of sediment production to the stream from these treated slopes was observed. The workmanship and construction are sturdyand of high quality. Grade A. { Since we visited Ah Pah Crk. the day after the RNP bypass failure, the stream was loaded with suspended sediments) 1990 - Review Comments- Bluff Creek ( 11022, 23, 24, 31, 32-$ 212,000): Access provided through lower Bluff Crk's former barrier section is still passing adults and juveniles following the Feb. 1986 flood event. The boulder weirs and boulder clusters near the yearling rearing facility are providing limited spawning improvement, but they do contain pockets of gravel utilized by spawners. Both the weirs and clusters have provided some good quality summer rearing habitats, and also refuge areas during winter flows. Two cluster groups are now buried under large streambank failures. These events could have been exacerbated by the placement of the boulders too close to the now failed right bank. No large wood or brush cover elements were utilized in the structures, although some were available. Personnel explained that the extreme velocities and power at high discharges prevented incorporating these organic components into their instream structures on Bluff Crk, Grade C. Camp Creek ( 11029, 30-$ 125,000): Six boulder weirs were constructed by USFS to trap spawning gravels. Two of the six weirs are now scattered boulder clusters, having been rearranged by the stream. The surviving weirs have provided gravels and are being used by fish. The boulder groups, both designed and incidental, are providing some good quality rearing habitats and some pockets of gravel used for spawning salmonids. 3rade C. Cappell Creek ( 11027-$ 125,000): BIA artificial propagation project. Project has operated for one year. It has released 17,035 CWT Chinook. Typical of the lower river hatchery programs, securing desired numbers of late running chinook broodstocks is very difficult. A lot of money in terms of fry produced, but the facility start- up costs are now over and the annual cost will be much less than the initial investment. Grade C. Hunter Creek ( 11001, 11002, 11013-$ 19,328): A CCC, DFG, and Simpson project to improve Hunter Creek on a basin scale. CCC now have a thorough instream assessment and instream structure plan prepared by Clearwater Biostudies, inc. under contract to them. Instream structure work is now underway by CCC crews. The construction is of excellent quality and design. All upper stream barrier work is now completed. The dry lower reaches of the stream pose a dewatered, complete barrier to all adults running before early November in most years ( T. Payne, 1989). Some concern over future land management's effect on the stream in the event of a major flood occurrence. Grade B. McGarvey Creek ( 11025, 11014, 11003-$ 24,264): Status of the hatch box project is not known. The barrier work is all done and passing fish. Grade C. - Review Comments- Pecwan Creek ( 11021, 11036, 11028-$ 50,000): A total of 21,626 yearling chinook were released from 1982- 84 from this facility* They were from Iron Gate stocks and deemed not suitable for the restocking goals of the project area. Since 1985, the facility's production is not well documented, but 27,000 for the period 1985- 88 is estimated. None of the releases from this site have been CWT. The Pecwan site has been used as a broodstock source for Cappell Creek as well. Grade D. Red Cap Creek ( 11033, 34, 35-$ 70,000): USFS project has produced some impressive results. Failing banks have been armored and vegetated. A series of over thirty boulder weirs and clusters have provided some high quality spawning and rearing habitats. Large wood cover elements have been used somewhat in the project. The project reach is in a stream section of former generally poor habitats and low utilization by salmonids; they were abundant during our visits. There is a yearling pond adjacent to the treatment section. Grade A. Richardson Creek ( 11026-$ 25,200): This project removed a barrier to salmonids and is functional. Seemed expensive. Grade C. Salt Creek ( 11000, 11012-$ 18,944): CCC successfully stabilized failing banks. All barrier work is completed and functional. One of the few upslope erosion control projects in the review has controlled the sediment output from the roadway. There is a lot of product here for the money. Grade A. Surpur Creek ( 11005-$ 3,456): CCC removed barriers at a bargain price. Still functional. Grade A. Tarup Creek ( 11004, 11011, 11015, 16, 17-$ 77,024): CCC has a plan for the creek and instream treatments done under contract by Inter- Fluv Inc. The work outlined in the plan is now completed, and is of very high quality and design for the most part. The work involved barrier modification, instream structures, revegetation upslope as well in the riparian zone, and some upslope erosion control ( one site upslope was quite major, in fact). Tarup, regardless of all these improvements, has a low flow access problem in its delta. Grade B. Pine Creek ( 10019, 20-$- 0-): Not reviewed. Various streams ( 11019- 20-$ 550,000): This is the CCC operation fund for the Lower Klamath program. This ongoing general fund was not deemed suitable for field review or rating. However, our general observation of the CCC/ DFG Lower Klamath program has certainly produced a positive impression of their work and approach. - Review Comments- MIDDLE KLAMATH SUBBASIN: Beaver Creek ( 6000- 05, 6035, 6053, 6065, 6066-$ 124,400): The boulder cluster groups and weirs constructed on Beaver Creek are not well utilized at this time. Silts and sediments nave impacted the quality of the gravel associated with the structures to the extent that some cementing has occurred. Therefore, it is believed that utilization by spawners has also been effected. The structures designed for the provision of rearing habitats have done better, and some of course do both, some neither. Grade C, The rearing facility ( 6035) was closed in 1985, but there is now talk of re- opening it. 1980- 84 releases averaged 29,423 yearling chinook of Iron Gate origin. Grade C. The gravel seeding occurred in 1985 ( 6052) and no evaluation was considered possible in 1989, nor was any proffered by staff. The two screens ( 6065- 66) are functional, but require regular upkeep and periodic thorough maintenance. Grade B. Bluff Creek ( 6036-$- 0-): This is one of the Klamath system's highest production cooperative rearing facilities. It has averaged 66,462 chinook yearlings for the past three years. These fish are of Iron Gate origin. Although adult runs are up in Bluff Creek, there is little baseline data, and until the current brood no CWT's were done on the ponded fish. Grade B. Bogus Creek ( 6046- 47, 6053- 54, 6061-$ 94,750): Bogus Creek is heavily utilized by naturally spawning chinook of Iron Gate Hatchery origin as well as by stocks of its own. The projects designed to provide more and/ or better gravels for these fish have met with apparent success, since in almost all cases the projects are used by the spawners, but so is everything else. What that means in real incremental gains that can be credited to particular habitat treatments is therefore difficult to assess. CWT and DSM evaluation programs are ongoing. Grade C. Camp Creek ( 6037-$- 0-): This rearing facility switched from Iron Gate chinook stocks to natal stocks in 1987. Yearling releases dropped from an average of 27,533 to 14,573 after the change. This can be attributed to the difficulty in trapping adults in an open, high discharge system. Still, the fact that they are now utilizing later running stocks that are adapted to Camp Creek's flow regime and conditions counts for a great deal. The natal brood have been marked with alternating maxillary clips ( right one year, left the next) prior to release and some have been recovered as adults. Grade B+. China Creek ( 6008- 09-$ 9,300): Not reviewed. Report is that the access is good throughout the stream now. No report on the status of the structures. - Review Comments- Clear Creek ( 6010, 6068- 69-$ 66,400): Fish and Game's barrier removal is providing access successfully. Report is that access is good throughout Clear Creek at this time. Grade B. Coon Creek ( 6056-$ 30,000): This ladder passes steelhead, but DFG is not certain about coho. It also requires some light upkeep. Grade B. Cottonwood Creek ( 6049-$ 22,966): Gravel placed on these weirs needs to be re- seeded periodically at the cost of $ 2,000 each time. Grade D. ( 6057-$ 6,000): Not reviewed. ( 6055-$ 5,000): Ladder is on line and working well. Grade B. ( 6058- 60-$ 29,500): These screens are all on line and operational, but require light periodic maintenance which is conducted by the Yreka Screen Shop on a rotating basis. Grade B. ( 6070-$ 1,200): The potholes blasted to trap gravel have trapped sand instead, so the goal of creating spawning habitat was not met. However, fry usage and survival seem to be good in the resultant pools. Not a high cost project. Grade C. ( Total Cottonwood Creek budget: $ 64,666) Di1lon Creek ( 6071-$ 5,000): This functional project opened five miles of good habitat now utilized by steelhead and Chinook. Grade A. Doolittle Creek ( 6011-$ 2,300) : The treated log jam has not reformed and access is still good for steelhead. Grade C. Elk Creek ( 6012- 14-$ 41,000): The boulder weirs and clusters are now all installed and need flows for evaluation of performance. ( 6034, 6045-$ 10,000) : The washout pond has averaged 31,205 released Iron Gate chinook yearlings since 1984. Grade B. ( Total Elk Creek budget: $ 51,000) Grider Creek ( 6015- 16, 6038-$ 18,500): The falls are now passing fish successfully. Grade A. The boulder weirs have been successful in trapping spawning gravel and are being used by chinook. Grade A. The ponds have grown an average of 34,426 Iron Gate chinook yearlings since 1987. Grade B. Horse Creek ( 6062- 64, 6074-$ 35,000): The three screens are installed and operational, but require light maintenance. Yreka Screen Shop provides this on an alternating basis. Grade B. The log jam is no longer an access problem. Grade A. ( Extant diversion dam is a major problem on this creek) Humbug Creek ( 6017- 18-$ 5,300): The boulder weirs are not successful and are physically failing. Grade F. The log weirs have worked well and are providing spawning and rearing habitat. Grade A. In any event, ten miles of good quality habitat are blocked to salmonids by dredge tailings in lower Humbug Creek. - Review Comments- Independence Creek ( 6019-$ 5,000): The stream's mouth is still open and fish access it. Grade B. Indian Creek ( 6006, 6020- 28, 6039- 40, 6067, 6072~$ 200,600): AH modified former barriers are now passing fish. Grade A. The recent instream structures all appear to be performing to design; biological evaluation is underway now. Grade B. The spawning channel is used extensively by steelhead, and to a lesser extent by coho, but not by chinook. It is also a maintenance item ( ie. supplemental gravel). Grade D. The rearing ponds have averaged 74,134 Iron Gate yearlings since 1985. Grade B. Irving Creek ( 6029-$ 9,300): The use of small boulders to construct inadequately sized structures resulted in no net gain from this project. Grade F. Iron Gate Hatchery ( 6033-$-?-): The hatchery is modifying its operations to better cope with problems associated with temperatures, density, and release timing according to the hatchery manager. Grade C. Badger Flat and Tree of Heaven ( 6050- 51-$ 136,000): These spawning channels have both been unsuccessful due to design flaws. They require constant maintenance which is not possible during usage. Gravel seeding is an ongoing project. Grade F. Little Bogus Creek ( 6048-$ 20,000): These seeded weirs were not reviewed, but they are reported to be intensely utilized by spawners. However, some maintenance is also required. Pearch Creek ( 6041-$- 0-): These ponds are operated by the Orleans Rod and Gun Club and have good public involvement and educational value. About 9,000 steelhead of Salmon River origin are reared here. A lot of enthusiasm and local stocks. Grade A. Red Cap Creek ( 6042-$- 0-): This rearing pond has averaged 37,862 Iron Gate chinook yearlings since 1985 and is operated in a system that has also had significant habitat improvement projects recently completed. A CWT program would help evaluate both of these aspects of the Red Cap Creek endeavor. Grade B. Seiad Creek ( 6030- 31, 6073-$ 5,100): The barrier project has been successful. Grade A. The weir projects were not found and therefore not reviewed. Thompson Creek ( 6032, 6043-$ 5,000): The rearing ponds were closed in 1985. The instream structures were not reviewed. West Branch Creek ( 6007-$ 5,500): The weirs are used by steelhead for spawning, according to local observers; they seem functional. Grade C. - Review Comments- Wilson Creek ( 6007-$- 0-): This private rearing facility was not reviewed. According to locals, it is not in use at this time. SALMON RIVER: Black Bear Creek ( 5000-$ 11,000): This USFS project successfully provided access for steelhead into the creek, and it is currently being utilized. Grade A. Kelly Gulch ( 5002- 03-$ 9,500): This project was not reviewed, but USFS staff reported that the barrier was still not passing all fish attempting to access the system. Their evaluation is underway now. Knownothing Creek ( 5004- 06, 5021-$ 153,114): The removal of the diversion dams and other barriers resulted, in doubling the chinook and coho runs into the creek. Grade A. The weirs ( 5006) were not completed at the time of the review. Delays were incurred because the rock was overshot resulting in boulders too small for the structures. Grade F. Nordheimer Creek ( 5007, 5008-$ 90,000): The log weirs ( 5007) failed. Grade F. The fishway ( 5008) is successful and passing fish. Grade A. Salmon River ( 5023, 5024-$ 8,000): This selective barrier was modified at a very reasonable cost and has improved access for al1 fish. Grade A. East Fork Salmon River ( 5013-$ 60,000): This project was not reviewed; USFS is evaluating now. South Fork Salmon River ( 5009- 12, 5014- 15, 5022, 5001-$ 176,200): ( 5009) This natal stock bioenhancement facility was located at a site with poor water temperature conditions for intense fish culture. Broodstock acquisition was also very difficult. The facility is now closed ( equipment will be relocated in the watershed, if possible). The project released 36,667 natal chinook smolts in the period from 1985 to 1987. Grade D. The boulder group projects were undergoing evaluation during the review period for biological response. The initial physical evaluation was not conclusive because many of the projects had not been subject to higher flows. Grade C. ( 5022) The " rough passage" area currently allows fish to pass without undue struggle. Grade B. ( 5001) The Blind Horse Creek weirs have not all been successful in providing spawning habitat. Many are trapping silt rather than spawning gravel. Rearing habitats are being provided by most of them, however. Grade D. - Review Comments- Specimen Creek ( 5016-$ 500): Steelhead now pass the treated log jam barrier. Another jam has formed above this site and requires monitoring and possible modification. Grade B. St. Claire Creek ( 5017- 20-$ 15,000): Steelhead now pass the modified barrier. The log weirs are holding gravel and in use by spawners. Juvenile cover is good associated with the weirs as well as the cover elements used in the project. The boulder weirs and clusters are also in place and in use. Grade A. SCOTT RIVER: Scott River and tribs. ( 4031- 4334 [ not inclusive]-$ 2, " 15,810) : These Soil Conservation District projects primarily involved placing rip- rap armor at 304 different sites in the upper Scott system. Not all were reviewed, and although the rock is stable and in place, many were found to lack streamside vegetation that would provide important shade and cover for the stream and aquatic life. Some others were buried in decomposed granite, sand or silt and therefore had little benefit for fish by way of providing complex micro- habitats. The value of these projects would be much greater if some of these items were addressed. Grade C. French Creek ( 4001, 4016- 18-$ 32,100): The sediment check dam initially filled in one storm event. It was excavated but refilled during the next runoff event. A high maintenance approach that treats the symptoms of the watershed's chronic erosion problem. Grade F. The screens are all in place and functional, but are dependent upon periodic light upkeep provided by the Yreka Screen Shop. Grade B. Kelsey Creek ( 4002- 04-$ 147,500): The weirs work well and are used by all species for spawning and rearing. Grade A. The USFS spawning channel has not performed as hoped. Problems have occurred relating to channel liner failure. The average number of pairs using the channel during the period 1985- 88 were: nine chinook, three coho, and twelve steelhead. In 1989 no usage was observed. It is also a very costly installation. Grade D-. Kidder Creek ( 4020- 21-$ 26,000): Both screens are in place and functional, but are dependent upon periodic maintenance provided by the Yreka Screen Shop. Grade B. Patterson Creek ( 4019-$ 9,000): This screen is in place and functional, but is dependent upon periodic maintenance provided by the Yreka Screen Shop. Grade B. - Review Comments- Scott River ( 4005- 06, 4012- 15-$ 94,800): Although the gravels were ' cleaned' the sedimentation problem returned the next year, This treatment does not address the problem, but rather the symptoms and would require constant maintenance. Grade F. The boulder groups were not installed after gauging the rapid sedimentation rate. The four screens are in place and functional, but are dependent upon periodic maintenance provided by the Yreka Screen Shop. Grade B. East Fork Scott River ( 4010- 11-$ 20,000): These two screens are in place and functional, but are dependent upon periodic maintenance provided by the Yreka Screen Shop. Grade B. Shakleford Creek ( 4009, 4022- 4030 incl., 4323, 4329-$ 343,720): ( 4009) The bank armor was not surveyed, but is reported to be stabilizing the soft banks. The fishery benefits are not known, ( 4022- 30) These nine screens are in place and functional, but are dependent upon periodic maintenance provided by tne Yreka Screen Shop, Grade B. ( 4323, 4329) The rip- rap bank armor is in place, but needs vegetation and cover elements added to increase fishery values. Grade C. Thomkins Creek ( 4007- 08-$ 6,500): The weirs are installed but are not highly utilized because of the recruited fine sediments now accumulated on them. Grade D. The fishway has provided access and is currently functional. Grade B. SHASTA RIVER: Parks Creek ( 3018-$ 42,000): These four screens are in place and functional, but are dependent upon periodic maintenance provided by the Yreka Screen Shop. Grade B. Shasta River ( 3000- 04, 3005- 08, 3009- 17-$ 519,000): ( 3000- 04) These weirs have deteriorated over the past few years due to the use of undersized boulders in construction. Only about 10% of the effective structures remain. In 1989 only 32 redds were observed on the weirs. Very expensive ($ 363,000) spawning gravel. Grade D. The four fishways ( 3005- 08-$ 17,000) are all currently passing fish. Grade B. The nine screens ( 3009- 17-$ 139,000) are in place and functional, but are dependent upon periodic maintenance provided by the Yreka Screen Shop. Grade B. 12 0140402500 UPPER KLAMATH RIVER: Fal1 Creek ( 2000-$- 0-): The Fall Creek hatchery facility is on line and ready to augment Iron Gate's production. The site has very good water quality and can be instrumental in relieving crowding problems at Iron Gate.

1516. [Image] Crater Lake limnological studies: final report


	ill., maps; July 1993."; "Cooperative Park Studies Unit, College of Forestry, Oregon State University."; Includes bibliographical references.; This title is a culmination of the first 10-years of the Crater ...
	Citation Citation Citation Abstract Copy Title: Crater Lake limnological studies: final report Author: Gary L. Larson; McIntire, David C.; Jacobs, Ruth W; Year: 1993, 2009 ill., maps; July 1993."; "Cooperative Park Studies Unit, College of Forestry, Oregon State University."; Includes bibliographical references.; This title is a culmination of the first 10-years of the Crater Lake limnological studies and a long-term monitoring proposal to investigate new hypotheses. Title: Crater Lake limnological studies: final report Author: Gary L. Larson; McIntire, David C.; Jacobs, Ruth W; Year: 1993, 2009 ill., maps; July 1993."; "Cooperative Park Studies Unit, College of Forestry, Oregon State University."; Includes bibliographical references.; This title is a culmination of the first 10-years of the Crater Lake limnological studies and a long-term monitoring proposal to investigate new hypotheses.

1517. [Image] Region II Klamath Project annual history, 1945


	Ill., maps (some color), photographs; Includes fiscal year financials, photographs, crop and livestock yields, water storage and distribution, hydrography report, etc.; Title covers: calendar years for ...
	Citation Citation Citation Abstract Copy Title: Region II Klamath Project annual history, 1945 Author: United States. Bureau of Reclamation Year: 1945, 2008 Ill., maps (some color), photographs; Includes fiscal year financials, photographs, crop and livestock yields, water storage and distribution, hydrography report, etc.; Title covers: calendar years for 1944 – 1945; Description is based on: Region II Klamath Project annual history 1944. Contains three parts and three table of contents.; Dates of the beginning year(s) of publication are derived from May 1, 1903 to December 31, 1912, History of the Klamath Project and from the volume information on later volumes (v. 35) Klamath District and Klamath Project Annual history for 1945, dated December 1, 1946 Title: Region II Klamath Project annual history, 1945 Author: United States. Bureau of Reclamation Year: 1945, 2008 Ill., maps (some color), photographs; Includes fiscal year financials, photographs, crop and livestock yields, water storage and distribution, hydrography report, etc.; Title covers: calendar years for 1944 – 1945; Description is based on: Region II Klamath Project annual history 1944. Contains three parts and three table of contents.; Dates of the beginning year(s) of publication are derived from May 1, 1903 to December 31, 1912, History of the Klamath Project and from the volume information on later volumes (v. 35) Klamath District and Klamath Project Annual history for 1945, dated December 1, 1946

1518. [Image] Federal Register - Endangered and Threatened Wildlife and Plants; Notice of 90-Day Finding on a Petition to Delist the Lost River Sucker and Shortnose Sucker


	Only portions of issues of the Federal Register are available in the Klamath Waters Digital Library. Includes bibliographical reference; 50 CFR Part 17; Action: Notice of 90-day petition finding; “FR Doc. ...
	Citation Citation Citation Abstract Copy Title: Federal Register - Endangered and Threatened Wildlife and Plants; Notice of 90-Day Finding on a Petition to Delist the Lost River Sucker and Shortnose Sucker Year: 2002, 2008, 2005 Only portions of issues of the Federal Register are available in the Klamath Waters Digital Library. Includes bibliographical reference; 50 CFR Part 17; Action: Notice of 90-day petition finding; “FR Doc. 02-12123 Filed 5-13-02: 8:45 a.m.;” See the Federal Register at http://www.gpoaccess.gov/fr/advanced.html Title: Federal Register - Endangered and Threatened Wildlife and Plants; Notice of 90-Day Finding on a Petition to Delist the Lost River Sucker and Shortnose Sucker Year: 2002, 2008, 2005 Only portions of issues of the Federal Register are available in the Klamath Waters Digital Library. Includes bibliographical reference; 50 CFR Part 17; Action: Notice of 90-day petition finding; “FR Doc. 02-12123 Filed 5-13-02: 8:45 a.m.;” See the Federal Register at http://www.gpoaccess.gov/fr/advanced.html

1519. [Image] Forest conditions in the Cascade Range Forest Reserve, Oregon


	Subject series H. Forestry 6
	Citation Citation Citation Abstract Copy Title: Forest conditions in the Cascade Range Forest Reserve, Oregon Author: Geological Survey (U.S.) Year: 1903, 2007 Subject series H. Forestry 6 Title: Forest conditions in the Cascade Range Forest Reserve, Oregon Author: Geological Survey (U.S.) Year: 1903, 2007 Subject series H. Forestry 6

1520. [Image] The Water Report. Klamath Fishery Science: Controversy in the Klamath River Basin


	Only portions of issues of The Water Report are available in the Klamath Waters Digital Library. Includes bibliographic references. See the full report at http://www.thewaterreport.com/.
	Citation Citation Citation Abstract Copy Title: The Water Report. Klamath Fishery Science: Controversy in the Klamath River Basin Author: Envirotech Publications Year: 2005, 2008, 2006 Only portions of issues of The Water Report are available in the Klamath Waters Digital Library. Includes bibliographic references. See the full report at http://www.thewaterreport.com/. Title: The Water Report. Klamath Fishery Science: Controversy in the Klamath River Basin Author: Envirotech Publications Year: 2005, 2008, 2006 Only portions of issues of The Water Report are available in the Klamath Waters Digital Library. Includes bibliographic references. See the full report at http://www.thewaterreport.com/.

1521. [Image] Soil survey of Crater Lake National Park, Oregon


	ill. (some col.), maps (some col.); 13 folded maps tipped in; Also available via Internet as of April 20, 2005; Includes data tables; Includes bibliographical references (p. 151-153) and glossary (p. 1...
	Citation Citation Citation Abstract Copy Title: Soil survey of Crater Lake National Park, Oregon Author: United States Department of Agriculture, Natural Resources Conservation Service, in cooperation with United States Department of the Interior, National Park Service Year: 2008 ill. (some col.), maps (some col.); 13 folded maps tipped in; Also available via Internet as of April 20, 2005; Includes data tables; Includes bibliographical references (p. 151-153) and glossary (p. 155-163) Title: Soil survey of Crater Lake National Park, Oregon Author: United States Department of Agriculture, Natural Resources Conservation Service, in cooperation with United States Department of the Interior, National Park Service Year: 2008 ill. (some col.), maps (some col.); 13 folded maps tipped in; Also available via Internet as of April 20, 2005; Includes data tables; Includes bibliographical references (p. 151-153) and glossary (p. 155-163)

1522. [Image] Trinity River Flow Evaluation: final report: a report to the Secretary , U.S. Department of the Interior


	TRINITY RIVER FLOW EVALUATION - FINAL REPORT EXECUTIVE SUMMARY When Congress authorized construction of the Trinity River Division (TRD) of the Central Valley Project (CVP) in 1955, the expectation was ...
	Citation Citation Citation Abstract Copy Title: Trinity River Flow Evaluation: final report: a report to the Secretary , U.S. Department of the Interior Author: U.S. Fish and Wildlife Service; Arcata Fish and Wildlife Office; Hoopa Valley Tribe Year: 1999, 2006, 2005 TRINITY RIVER FLOW EVALUATION - FINAL REPORT EXECUTIVE SUMMARY When Congress authorized construction of the Trinity River Division (TRD) of the Central Valley Project (CVP) in 1955, the expectation was that surplus water could be exported to the Central Valley without harm to the fish and wildlife resources of the Trinity River. The TRD began operations in 1963, diverting up to 90 percent of the Trinity River's average annual yield at Lewiston, California. Access to 109 river miles of fish habitat and replenishment of coarse sediment from upstream river segments were permanently eliminated by Lewiston and Trinity Dams. Within a decade of completing the TRD, the adverse biological and geomorphic responses to TRD operations were obvious. Riverine habitats below Lewiston Dam degraded and salmon and steelhead populations noticeably declined. In 1981, the Secretary of the Interior (Secretary) directed that a Trinity River Flow Evaluation (TRFE) study be conducted to determine how to rest Title: Trinity River Flow Evaluation: final report: a report to the Secretary , U.S. Department of the Interior Author: U.S. Fish and Wildlife Service; Arcata Fish and Wildlife Office; Hoopa Valley Tribe Year: 1999, 2006, 2005 TRINITY RIVER FLOW EVALUATION - FINAL REPORT EXECUTIVE SUMMARY When Congress authorized construction of the Trinity River Division (TRD) of the Central Valley Project (CVP) in 1955, the expectation was that surplus water could be exported to the Central Valley without harm to the fish and wildlife resources of the Trinity River. The TRD began operations in 1963, diverting up to 90 percent of the Trinity River's average annual yield at Lewiston, California. Access to 109 river miles of fish habitat and replenishment of coarse sediment from upstream river segments were permanently eliminated by Lewiston and Trinity Dams. Within a decade of completing the TRD, the adverse biological and geomorphic responses to TRD operations were obvious. Riverine habitats below Lewiston Dam degraded and salmon and steelhead populations noticeably declined. In 1981, the Secretary of the Interior (Secretary) directed that a Trinity River Flow Evaluation (TRFE) study be conducted to determine how to rest

1523. [Image] Agricultural information on Klamath County irrigation


	Pamphlet, compiled by the Klamath County Agricultural Agent, describing the history and status of the Klamath Project
	Citation Citation Citation Abstract Copy Title: Agricultural information on Klamath County irrigation Author: Henderson, C.A. Year: 1930, 2005 Pamphlet, compiled by the Klamath County Agricultural Agent, describing the history and status of the Klamath Project Title: Agricultural information on Klamath County irrigation Author: Henderson, C.A. Year: 1930, 2005 Pamphlet, compiled by the Klamath County Agricultural Agent, describing the history and status of the Klamath Project

1524. [Image] Ecology of shortnose and Lost River suckers in Tule Lake National Wildlife Refuge, California : progress report, April - November 1999


	Ecology of shortnose and Lost River suckers in Tule Lake National Wildlife Refuge, California, Progress Report, April - November 1999 Lisa A. Hicks, U. S. Fish and Wildlife Service, Klamath Basin National ...
	Citation Citation Citation Abstract Copy Title: Ecology of shortnose and Lost River suckers in Tule Lake National Wildlife Refuge, California : progress report, April - November 1999 Author: Hicks, Lisa A.; Mauser, David M.; Beckstrand, John; Thomson, Dani Year: 2000, 2005 Ecology of shortnose and Lost River suckers in Tule Lake National Wildlife Refuge, California, Progress Report, April - November 1999 Lisa A. Hicks, U. S. Fish and Wildlife Service, Klamath Basin National Wildlife Refuge, Route 1, Box 74, Tulelake, CA 96134 David M. Mauser, U. S. Fish and Wildlife Service, Klamath Basin National Wildlife Refuge, Route 1, Box 74, Tulelake, CA 96134 John Beckstrand, U. S. Fish and Wildlife Service, Klamath Basin National Wildlife Refuge, Route 1, Box 74, Tulelake, CA 96134 Dani Thomson, U. S. Fish and Wildlife Service, Klamath Basin National Wildlife Refuge, Route 1, Box 74, Tulelake, CA 96134 Introduction The Lost River ( Deltistes luxatus) and shortnose ( Chasmistes brevirostris) suckers were federally listed as endangered species on July 18, 1988 ( Federal Register 53: 27130- 27134). Both sucker species are relatively long- lived, have a limited geographic range, and are endemic to the Upper Klamath Basin of Northern California and Southern Oregon. Habitat degradation from water diversions and loss of riparian and wetlands habitats associated with agricultural development within their historic range is believed to be the major reason for the species decline ( U. S. Fish and Wildlife Service 1993). A more detailed description on the life history, habitat requirements, and causes of decline of the species can be found in the Lost River and Shortnose Sucker Recovery Plan ( U. S. Fish and Wildlife Service 1993). Tule Lake National Wildlife Refuge ( NWR), established in 1928, consists of 2 return flow sumps ( Sump 1( A) and 1( B)) totaling 13,000 acres surrounded by 17,000 acres of intensively farmed lands ( Fig. 1). The refuge and surrounding private agricultural lands occupy the historic lake bed of Tule Lake, a 95,000 acre lake and marsh area that was reclaimed in the early 1900fs as part of the Klamath Reclamation Project. Current management of the refuge is directed by the Kuchel Act of 1964 which mandates the refuge be managed for the major purpose of waterfowl management but with optimal agricultural use that is consistent therewith. Both sumps are shallow ( 0.1 - 2.0 m) and consist of approximately 10,500 acres of open water with a 2,500 acre shallow (< 0.1 m) emergent marsh at the northeast corner of Sump 1( A). Tule Lake has been identified as a potential refugia for both sucker species ( U. S. Fish and Wildlife Service 1993). Tule T like National Wildlife Sump 3 Lease lands Field . Station Cocbetative Fanning Fields Area J Lease Lands Sump 2 I ease I , ands Figure 1. Tule Lake National Wildlife Refuge, California. During winter, water within the sumps is comprised primarily of local runoff and during summer water is comprised primarily of irrigation return flows, originating from Upper Klamath Lake. Summer water quality in the sumps is similar to other water bodies within the Upper Klamath Basin and is considered hypereutrophic ( Dileanis et al. 1996). Water quality problems include low dissolved oxygen ( DO) and high hydrogen ion concentrations ( pH) and unionized ammonia. Water quality in the Tule Lake sumps is directly affected by hypereutrophic conditions in Upper Klamath Lake ( U. S. Fish and Wildlife Service 1993). Studies conducted after publication of the Shortnose and Lost River Sucker Recovery Plan indicate that Tule Lake contains an estimated 159 ( 95% CI = 48- 289) shortnose and 105 ( 95% CI = 25- 175) Lost River suckers ( Scoppetone and Buettner 1995). Confidence intervals for these estimates are large because of small sample sizes and low rates of recapture. Recruitment rates for the Tule Lake population via spawning below Anderson- Rose Dam is low with significant larval production occurring only in 1995 ( monitoring occurred 1991- 99) ( M. Buettner, pers. comm). Entrainment from the irrigation system is likely the largest source offish for Tule Lake ( U. S. Bureau of Reclamation 1998). Both species of suckers in Tule lake are in good physical condition relative to fish in Clear Lake and Upper Klamath Lake with Tule Lake fish being generally heavier and exhibiting few if any problems with parasites or lamprey. ( Scoppetone and Buettner 1995). U. S. Bureau of Reclamation ( Reclamation) biologists tracked 10 radio- marked suckers in Tule Lake from 1993- 95. From these studies, specific use areas by time period were identified with over 99% of radio locations occurring in Sump 1( A). Of particular importance from these studies was identification of an over- summer site in the south central region of Sump 1( A) termed the ADonut Hole# ( DH). In early 1999, the U. S. Fish and Wildlife Service ( Service) proposed a wetland enhancement project on the 3,500 acre Sump 1( B). The project was designed to improve habitat for waterfowl and other associated wetland species as well as improve water quality through the conversion of Sump 1( B) from an open body of shallow water to an emergent year- round flooded wetland. The primary mechanism to create the desired habitat condition is a series of annual spring/ summer drawdowns thereby creating conditions suitable for germination of desired emergent plant species. Of principal concern in developing the project was the potential effects on suckers within the sumps. Because of the proximity of both sucker species in adjacent Sump 1( A), a project monitoring plan was developed to ascertain the potential effects of the Sump 1( B) Project on suckers and water quality. Our monitoring design benefitted from studies of water quality and sucker movements by Reclamation biologists from 1992- 95. This report summarizes findings of the first year= s pre- project monitoring effort ( April- December, 1999) relative to water quality and movements of radio- marked suckers. Objectives 1. Describe seasonal distribution and movement patterns of both sucker species in Tule Lake NWR and determine if fish movements have changed since initial studies by Reclamation biologists in 1993- 95. 2. Characterize water quality, in space and time, of areas used by adult suckers compared to areas which are not used. 3. Document and describe movements of radio- marked suckers to spawning areas below Anderson- Rose dam. 4. Determine whether recruitment of larvae and juvenile was occurring below Anderson- Rose Dam. Methods Monitoring radio- marked adult suckers In April and May, 1999, Reclamation biologists captured 14 suckers and surgically implanted radio- transmitters ( ATS, Isanti, MN) having a projected battery life of 12 months. Each transmitter had an external antennae that exited the body cavity near the lateral line of the fish. Eleven Lost River and 3 shortnose suckers were captured using trammel nets at the northwest corner of Sump 1( A) ( 9 fish) and immediately downstream of Anderson- Rose Dam on the Lost River ( 5 fish) ( Table 1). We located radio- marked fish via air thrust boats using a scanning receiver and 4- element yagi antennae. Fish were located fish 4 times/ month during March and April, 2 times/ month from May through September, and once per month from October through December. Fish not located via boat were located from fixed wing aircraft. We determined fish locations by moving as close as possible to undisturbed fish and recording locations with a Global Positioning System ( GPS). All GPS positions consisted of 180 rover points/ location and were differentially corrected via post processing software ( PFinder ver. 2.11). We recorded depth information at each fish location. To determine timing and duration of the spawning migration, we monitored radio-marked fish from vehicles on the east levee of the Lost River downstream of Anderson- Rose Dam. Table 1. Data from Lost River and shortnose suckers captured on Tule Lake National Wildlife Refuge, California and Anderson- Rose Dam, Oregon in 1999. RADIO TAG 165.043 165.063 165.073 165.103 165.084 165.094 164.641 164.863 164.494 164.854 165.054 164.845 164.763 164.914 CAPTURE DATE 4/ 2/ 99 4/ 2/ 99 4/ 2/ 99 4/ 2/ 99 4/ 2/ 99 4/ 2/ 99 4/ 9/ 99 4/ 2/ 99 4/ 9/ 99 4/ 30/ 99 5/ 5/ 99 5/ 5/ 99 5/ 18/ 99 5/ 18/ 99 CAPTURE LOCATION TULELAKE SUMP1A TULELAKE SUMP 1A TULELAKE SUMP 1A TULELAKE SUMP 1A TULELAKE SUMP1A TULELAKE SUMP 1A TULELAKE SUMP1A TULELAKE SUMP1A TULELAKE SUMP 1A ANDERSON ROSE DAM ANDERSON ROSE DAM ANDERSON ROSE DAM ANDERSON ROSE DAM ANDERSON ROSE DAM SPECIES LOST RIVER LOST RIVER LOST RIVER SHORTNOSE SHORTNOSE LOST RIVER SHORTNOSE LOST RIVER LOST RIVER LOST RIVER LOST RIVER LOST RIVER LOST RIVER LOST RIVER SEX FEMALE FEMALE FEMALE MALE FEMALE FEMALE FEMALE MALE FEMALE FEMALE MALE MALE MALE FEMALE WEIGHT NO DATA NO DATA NO DATA NO DATA NO DATA NO DATA 2830 g 1040 g 5260 g NO DATA 2214 g 1542g 2350 g 1811 g FORK LENGTH 777 mm 681 mm 754 mm 473 mm 523 mm 754 mm 544 mm 440 mm 775 mm 753 mm 556 mm 486 mm 594 mm 477 mm PIT TAG NO. 1F3E34432C 1F39064959 1F4C5A6754 1F07315752 1F31462743 1F4C5A6754 1F3726750F 1F36490062 1F37103466 1F390F1801 1F3E2A7702 1F36443235 1F30753309 1F390E6B2F Recruitment Reclamation biologists conducted larval and juvenile sucker surveys during May and June by sampling, visually and with dip nets, the emergent vegetation at the periphery of the Lost River downstream of Anderson- Rose Dam. Egg viability surveys were conducted in the gravel sediments immediately below the dam in May. Water quality We preselected water quality sampling sites ( Fig. 2, Table 2) in Sump 1( A) to correspond to adult sucker use areas as determined by studies of radio- marked adult suckers conducted by Reclamation in 1993- 95 ( Fig. 3). We selected 2 sites in Sump 1( B) which met or exceeded the minimum depth requirement (> 3ft) for both sucker species ( M. Buettner, pers. comm.) after referring to 1986 bathymetric maps. We attempted to obtain data from each site twice/ month. We moved 2 sample sites ( Donut Hole and Donut Hole Northwest) early in the summer and 1 site ( Donut Hole West) ( Fig. 2) during mid- summer to better represent summer use locations of radio- marked fish. From May through November, we measured water quality parameters ( dissolved oxygen ( DO), hydrogen ion concentration ( pH), and temperature (° C)) using DataSonde 3, 4 and 4a= s ( Hydrolab Corp., Austin, Texas) ( hereafter referred to as Hydrolabs) 26 cm ( 12 in) above the sediment. We suspended Hydrolabs, within PVC tubes, from metal fence posts driven into the sediment. Data were collected hourly over a 96 hr period at each monitoring site. We downloaded data from Hydrolabs using the Hyperterminal software package v. 690170 to a personal computer. Unit probes were cleaned and calibrated according to Hydrolab guidelines ( Hydrolab Corporation 1997) and local geographic standards. Using the same deployment schedule as with our Hydrolabs, we sampled turbidity at each site using a Portable Turbidimeter model 21 OOP ( Hach Corp., P. O. Box 389, Loveland, CO 80539). We collected water samples 27 cm ( 12 in) above the sediment at each sample site. We measured turbidity in NTUs, following the guidelines in the product manual and we measured water depth using a hand- crafted wooden pole, marked in measured increments. We summarized water quality data using Microsoft 8 EXCEL software v. 97 SR- 1 and SPSS for Windows release 9.0.0. Because of the apparent difference in summer water quality in the DH versus other sampling sites, data were summarized as DH sites and Non- DH ( NDH) sites. Tule Lake NWR Water Quality Monitoring 1999 MfSVTHOLE \ OKTIIH ' w Background Hvdrolon> Luke m Mudflats Uplands X Water Vionitonny Stations ( Hydrolafa sites) MK ker Radio \ ckmcin L. Hicks. D. .1 Beckitraod, K Miller, USFWS Background HydfOlOf} Sat'I Wetlands Invcnlon LSI Sh S Map Projection UTMZCM IO, WGS-* 4 By: L. Hkks. USFWSUSBR 02/ 00 i Figure 2. Water quality sample sites, Tule Lake National Wildlife Refuge, California, 1999. 8 Table 2. Characteristics of water quality sampling sites, Tule Lake National Wildlife Refuge, Tulelake, California, 1999. SITE NAME NORTHWEST SUMP 1A DONUT HOLE NORTHWEST DONUT HOLE WEST DONUT HOLE SOUTH DONUT HOLE DONUT HOLE EAST ENGLISH CHANNEL WEST SUMP IB EAST SUMP IB PUMP 10 SUMP 1A2 SITE ABBREVIATION NWS1A DHNWSlAor DHNW DHWEST DHSOUTH DHSlAorDH DHEAST ECSlAorEC WS1B ES1B PMP10 UTM N 4642199 4638316 4638881 4638144 4637299 4639024 4634604 4634153 4633948 4636635 UTME 620803 620542 321022 621355 621475 621971 625041 636647 628835 624748 DEPTH of MONITORING SITE ( m) 1 1.2 0.9 0.9 0.8 0.7 0.8 0.8 1.0 0.8 0.5 1 Depth of water at deployment 2 Pump 10 data will not be discussed in this document. Results Radio- marked suckers We located fish 231 times in locations similar to those determined by Reclamation biologists in 1993- 95 ( Figs 3- 4). Lost River and shortnose suckers did not appear to differentiate use of the sump by species; we located both species intermixed throughout the monitoring period. With the exception DH and DHNW ( Fig. 2), water quality sampling sites were close to seasonal sucker use areas. Of 14 suckers marked, mortality occurred in only 1 fish. A Lost River sucker (# X9) was tagged on 18 May at the Anderson Rose Dam; she was not located again until 23 days later on 9 June. From 9 June to 17 November, # X9 was located by signal within approximately 15 m of the original location based on the location data. It is likely that this fish died in early June within 2- 3 weeks of being radio- marked. It is unknown if this mortality was related to the stress of handling and marking or some other cause. April - May - In April- May, a period of maximum fish movements ( Figs. 5- 18), most suckers congregated in the AEnglish Channel ® between the sumps with a scattering offish located between the northwest corner of Sump 1( A) and the AEnglish Channel ® ( Fig. 4). Only 1 fish radio- marked in Tule Lake moved into the Lost River. This particular fish, a female shortnose sucker (# G9) was radio- marked in the northwest corner of Tule Lake on 9 April, was located in the AEnglish Channel ® on 14 April, and subsequently was located in Lost River below Anderson Rose Dam on 29 April and 6 May. Tule Lake Sucker Radio Telemetry \ pril 1993 - \! a> 1995 Hi tckwtstmd H) drohgy mm Marth/ Wi'lhiml • • River I Sucker Locations o Jan - Mar & Apr - May ° Jim - Sep • O t t - l h i 1 I . . . . . . ydtOl Ig) -: i '•'•, l: i M h - c .1 J I SI WS UtoBiihywwUy KkmrtiiB ••. iraOffia MapPinoiccii.- i rM2oni VM, S- » 4 • HJ I-. IKKV USffW& n SBB Figure 3. Locations of radio- marked suckers from studies conducted by U. S. Bureau of Reclamation, on Tule Lake National Wildlife Refuge, California, 1993- 1995. 10 Tule Lake NWR Sucker Radio Telemetry April - December 1999 Oregon California [ Sump 1A Background Hydrology J Lake Uplands SOcker Locations • Apr May o Jun - Sep • Oc! - Dec \| Qanuthole area = * 466 acres ( manually est from fish bca Suckei EUdiQ Tdctrcter: L Hi cks, D TtccnsDn, : Nati Wedatd^ Inventory. USTWS i t Hi cfa, usFwsnrsBH o 2/ 00 Figure 4. Locations of radio- marked suckers on Tule Lake National Wildlife Refuge, California, 1999. 11 Tule Lake- Sucker Radio Telemetr> - 1999 MMti « phrnl Fish: Lost River Sucker " A9" Sex Female Length: 777 mm fag I ocation I ulc I ; ike Sump IA Tai: Dare: 04/ 02 99 Vlort. Date: 3 - O 5 ni 0 5 - 1 ni ( Surface Fixation - 4034.9( 1') Lain' ihpth 1 - 15m Itydrolah tUm » t tm fcdarl .' i rein: l. llni. i. Becb- rmc l^ . I M I ^ I V I M . Kl; nn: nli limm Xvtup,- :, rr, k, I M •'• - \ * e BMb% « ldry KIWWHI I t em ,^ wnOi-... I SB I Background Hy* » : 4.. .. , „ \| WCIIWKIJ faivewior^. I'SI A S >• • ••• i •• i MZcne IC ' •..-• .: i;% i n . , i s , u s Figure 5. Movements of radio- marked sucker A9 on Tule Lake National Wildlife Refuge, California, 1999. 12 Tule Lake- Sucker Radio Telemetry ~- 1999 Hsh ], ost River Sucker"! Sc\ Female Length: UK] mm Tag Location [ We Lake Sump IA IML Dace U4/ O? W Mort Date: • i Khrr( m » depth) • 1 Mwrvl. Will. 1.1,1 I \|- l Muil I t * 3 - O 5 m 0 5 - t rn ( Surtax i: Nation - 4O34. W) flyJrttlaff SiKker RacfcTclemdn: I. IliduU. Bccks CompK. i BFW8 I. a.- Mil ,. l klmulklfaun \ « » OI.. . I MM Background llyfrotogv \ « bonB\| W ctlands inv « « or., U8FWS Map IVv^ vi ... i M ,. !• ' ••"• . I:-. \| \|\| ... i JFWS Figure 6. Movements of radio- marked sucker B9 on Tule Lake National Wildlife Refuge, California, 1999. 13 Tule Lake- Sucker Radio Telemetry - 1999 Fidi Lost River Sucker * C9" Sex Male Length: 619 mm Tag Location I ule Lake Sump IA Fag Date: M/ 02 w VIon. Date: { Surface Fixation - 4II34. W) tiat- ttffawmf th- frohf(\ • • Khii i> nJv\|> th) H i \ iM, vh\ wtl,..., i UplniKi Lak mm MU. I n. i 3 - 0 5 ni 0 5 - 1 ru • I n kaAo Tckwdn: LHkfcaJ. Beduimd P HMUWM K V'l « • .\|: I- II: I-\| I I n i ii Cwnpk. I 8FWS Klmwil.[ ten< •• . : M . . . I M : mind I l > * o t i c \ Ntttaaal Wetlands Inventory* I ^\| •.!•••• • • . • I -. I \ \| . , K 1 1 . i •• » •• -; !:•• I II . I SFWS r Mil . Figure 7. Movements of radio- marked sucker C9 on Tule Lake National Wildlife Refuge, California, 1999. 14 Tule Lake- Sucker Radio Telemetry - 1999 Haf kgnm n BB Rh « ' i MM. Fish Shortnose Sucker " l) l>" Sex Male Length: 473 nun ail Location: I ale Lake Sump IA Tag Date 04/ 02/ 99 Mort. Date: I Surface Fixation - 41> 34. lW) /....'.:• Depth Mi, I lbtx 0- OSm ^ ^ 0 5 - 1 rti - I - ' I •' • • ' ' • I HkfcU. lUbrxilHil) I ! . . . ! - . K Mil M KlttiHtfiBttk K « Aig « : . , - , - , L . I M ''. •• Ifydrolah Kit,-* i., i.- . il ... (.. , , , i , , •. . ; „ , . . , M ! - U a d ^ r t w n d ! ! > * • ••'• • t n \| XVctinjKlt [ mcTrt « . T\. • SFWS I • • . . • • , , • l:% \| n ...... i M A S * £> Figure 8. Movements of radio- marked sucker D9 on Tule Lake National Wildlife Refuge, California, 1999. 15 Tule Lake- Sucker Radio Telemetry - 1999 Fish Shortnose Sucker T39" Sc\ Female Length: 523 mm rag Location I ule I ake Sump IA rag Date M/ 02 w Date: • 1.1 I i) I 1-.. 1 • \| i i . . I. llcct. M m i l l ) ] Compl- • ' " I '• S 5> NJUOIWI Wetlands b i v c m u r y I IS I » S • ••• I " I ••. l/. nc It. i . . . : - . , ' II-. \| \|\| ..... Figure 9. Movements of radio- marked sucker E9 on Tule Lake National Wildlife Refuge, California, 1999. 16 Tule Lake- Sucker Radio Telemetry - 1999 Fish Lost River Sucker " IV Sc\ female Length: 754 mm Tag Location Tule Lake Sump 1A * rag Date 040; 99 Vkirt Date: ( Surface Fixation - 4( 134.90') Hat ground Hydrology U • : • • Rhtr< iM » < Jvpfh) • iM.., lll » r • i M. tvh\ VHl,, na 0.0,5m Uphml » 0S- 1rt. 1 - 1 5 IT » 1 £ m fackcrRadk> 1 r .. In: UfisfcaJ. Ikvkwjjjui P » •, K V, 1 • l: m: rli M a Jfcflifc* CorapUv I IFWS Uydrolth sit,- s i , i t \ t, il> m. f n Klmwlh tfewn .\ wn < » flfa . I SBR K o t o ^ : \ ai,,, na\| Wctljmd bivcm^ f • I SFWS Map hV^ vl .. . I MZpftClO Cony aid I;-, i n , . UWTOS Figure 10. Movements of radio- marked sucker F9 on Tule Lake National Wildlife Refuge, California, 1999. 17 Tule Lake- Sucker Radio Telemetry - 1999 Fish Shortnose Sucker " Q9" I cm ale Length: 544mm I. IL1 Location Tule Lake Sump IA * rag Date 04/ 09/ 99 Mori ( Surface rloaliun - I II . . I. \'-.-\-- m.' I-K V i ! l • l : n i : r l l ! - i i : ii : . r , : . \| , . I s\|\ VS KlmuHi Btom Aivs 4 M1K. I SBR \ j i > i m l Wetlands invcnlon i 5FWS M. « ;. ' - . . I - . I M / . „ . • \| » . I II , • I SFWS BB Ki^ i imi M \ hrvh\\ ilhiml Upland Lais Otfttk MuiJ Hals Figure 11. Movements of radio- marked sucker G9 on Tule Lake National Wildlife Refuge, California, 1999. 18 Tule Lake- Sucker Radio Telemetry ~ 1999 • Jit" Fish Sex Length: Tag Location: Tag Date: Sh oi1no so Male 440 mm Tule 1 < ikc 04/ 09/ 99 / Sucker Sump " H9" IA f tif( rtitiini / / i Kh< < 1- 1 . ri. l Mud FliitK 0 - 0 5 m 05 - 1 ni < SurfiKi 1 , - > 18m K V , , • l; , - n : , l , 5 , , , : . • „ • , '• • ' • • : ' k • ' s \| ' ' ' s K i i. l I-. . . . tVu. I M i ^ ' ^ \ tbonn\ Wetl « nd « faiv « mor>. I . \ I A • » - i I M „, \| i. Ih \| \|\| , , I M Figure 12. Movements of radio- marked sucker H9 on Tule Lake National Wildlife Refuge, California, 1999. 19 Tule Lake- Sucker Radio Telemetry - 1999 I- isii Lost River Sucker " 1 Sc\ Female Length: 775 mm Tag Location: Tule Lake Sump IA Tag Dale: 04/ 09/ 99 Mort. Date: ( Surface I* k^ atinn Tckmrtn: l.\|\| uk. I. K J y me l> I..: II> M K •-.•. I - I : . . , : Compkv • BPWS "' ••' Klmwlbl? ti » m A* MOffice I SBR IvckuioRv : \ atxin » l Wetlands biv « Mory. I > I / i < n k j f M U U l f i x • • • ' < • . • • Khri ( IM » tlr\|> rh) Mat vh Wit I HI ii I LpbmJ Figure 13. Movements of radio- marked sucker 19 on Tule Lake National Wildlife Refuge, California, 1999. 20 Tule Lake- Sucker Radio Telemetry - 1999 Fish: I- osi River Sucker " P9" Sc\ Female Length: 7^ ' m m lag Location Anderson Rose Dam Tag Dale: 04/ 30/ 99 Mort. Date: ( Surface bk'talkm - 4UJ4. W) % mkm i .' i eraetn: \|.\| ikk* J. lkvl> « uui I) . . . . i - K '•.'. . - i . . r . . i . BMte Rvtug « , « ., .. . . - . M V . . Compk. i IPWa I « l.- . ll ,. t ,.. , , , \| , , •. . „ ,. . \| M i • E* K* gr° umi I K v H , ^ htaHml Wctl » nd » knvMori i -- I - s ^ • •• I •• I M i . , - It. > •—•• . i;-. i II . . i MWN Figure 14. Movements of radio- marked sucker P9 on Tule Lake National Wildlife Refuge, California, 1999. 21 Tule Lake- Sucker Radio Telemetry - 1999 Fish Lost River Sucker " i;(>" Sex Male Length: 556mm Tag Location Anderson Rose Dam Tag Date 05 05 w Mort. Date: ( Surface H o at ion - - MM4. W) • i • i n. t . i. ikJ^•. m..- I) . M. HV. K Vi . • hnrnflh ii » m Hvfil^- '" I - I K ••. . I" K i r •• . M ... I MiM \-, ..,.•. \ , ,,.\| v. , \|,,.\|. ( r. v : , f . l MH • . ! ., I M „ \|. Figure 15. Movements of radio- marked sucker U9 on Tule Lake National Wildlife Refuge, California, 1999. 22 Tule Lake- Sucker Radio Telemetry - 1999 Fish: Lost River Sucker " W Sox: Male Leagth 486 mm \ AII Location; Anderson Rose Dam Tag Date: 05/ 05/ 99 Mort. Date: ( SurfiK- c Floaiiun 4 « . U. W\| •• ' • •• ' • ; • ' ' ' ' I I I . . • 1. Bedu HI.- D . K V I " , I . < l: iMi; iTh : - i • : .1 MIK! KI. HH I - • • > • . • • \ 1 i i i v . v l . r i l - i r . v : • ! • . 1 • . . . 1 . • 1 \ \| , , c 1. Figure 16. Movements of radio- marked sucker V9 on Tule Lake National Wildlife Refuge, California, 1999. 23 Tule Lake- Sucker Radio Telemetrv - 1999 Fish: Lost River Sticker " W(>" Sex: Male Length 594 nun I nil Location: Anderson Rose Dam Tag Date: 05/ 18/ 99 Meet. Date ( Surface H o at inn 4< i. U/) i » ') - ' • ' I ' : ' - ' • I Hid • i. Bcvl. v.' im: P . , i iikr. Klanwlh B oi R< tu^ : . . r v . k v I M •'•- ' -•• Mil - >•> • KlMmth IViim .\ wn 0 1 . . . I SBR g \ ^ m u l Wcllmls En^ :• r I ^ \| V \ • • • I - i I M/ V. u- It; 1 ••••:•• .-.' II-. W Figure 17. Movements of radio- marked sucker W9 on Tule Lake National Wildlife Refuge, California, 1999. 24 Tule Lake- Sucker Radio Telemetry - 1999 Fish: Lost River Sucker " X9" Sex: Female Length 477 mm Tag Location; Anderson Rose Dam Tag Date: 05,1899 Mori. Date, suspected in June 1999 Hn i in Mat h Will •. 1. fackn RadioTclenvtn; i. tfidbU. lkvk « ramLI>. r* Mmw « t K ','. . hmtdth B* m R^ UB* CompK- • n •'• • B % VJI < Kflb . I M i ,• h> tir> l Wetlands Envcntun. I SFft'S \ I , \ ' I K I I \| , ... \| s.\| , \ s Figure 18. Movements of radio- marked sucker X9 on Tule Lake National Wildlife Refuge, California, 1999. 25 June - September - During this period, nearly all suckers ( particularly during July and August) could be found in the DH at the south central portion of Sump 1( A) ( Fig. 4). By connecting the outermost locations of approximately 90% of radio locations, the calculated area of the DH was 188 ha. Suckers using the DH were found in depths ranging from 1.0- 1.3 m ( 39- 50 in) ( Fig. 19). September - December - During this period suckers moved from the DH to the northwest corner of Sump 1( A). As of the writing of this report, ( February 15, 2000) the 13 remaining fish occupy the same area. Recruitment Surveys by Reclamation biologists for larval and juvenile suckers in the Lost River below Anderson- Rose Dam failed to document the presence young of the year fish. Below is a summary of surveys: Date 5/ 25/ 99 6/ 2/ 99 6/ 10/ 99 Result Searches for eggs in gravel below Anderson- Rose Dam revealed eggs in 4 of 5 sites, some of which were viable. Larval surveys conducted at 3 sites ( visual and dip net) from the dam to the wooden bridge were negative. Larval surveys conducted at 5 sites including the dam, 2 and 1 mile downstream, the wooden bridge, and East- West Road were negative. Larval surveys conducted at 2 sites downstream of dam were negative. Water quality pHBln general, pH values were less variable in the DH then areas outside this region ( Fig. 20). In all areas, median pH values remained below 9.5 until early June at which time values outside the DH were frequently above 10.0. pH values were particularly high (> 10.0) in late June through August in ESIB and NWS1A and periodically in the EC and WS1B. pH values in the DH and areas adjacent, remained below 10.0 through September; however, there was a gradual rise in pH values in DH sites from May through September. In late September and early October, DH pH values exceeded all other sites. rem/ reratareBTemperatures in all regions reached a peak in late July through early August with no discernible difference between DH or NDH sites ( Fig. 21). Dissolved oxvgenBDonut Hole sampling station s differed in dissolved oxygen characteristics relative to other areas of the sumps. During the June through August period DH sites ranged from 4.5 to 11.2 mg/ 1 while areas outside this region ranged from 1.1 mg/ 1 to 18.2 mg/ 1 ( Fig. 21). Toward November DH and NDH sites became similar DO dynamics ( Fig. 21). 26 Turbiditvllln general, turbidity values appeared greater in the DH versus areas outside, although some sites particularly in Sump 1( B) were quite variable particularly in June and July. This may have been due to the large amount of filamentous algae in Sump 1( B), potentially interfering with the measurement. Turbidity rose sharply at sites by late October and November ( Fig. 23- 24). 20 >• 1 5 O UJ a UJ DC 10 0 39 41 43 45 47 More DEPTH Figure 19. Water depth used by radio- marked suckers in the " Donut Hole" ( June- August), Tule Lake NWR. California. 27 BJll I U r S o I! Figure 20. pH data collected from " Donut Hole" and non- Donut Hole water quality sampling sites on Tule Lake National Wildlife Refuge, California, 1999. Box and whisker plots represent the median, 25- 75* and 10- 90* percentiles, and outliers. 28 temp rC) S 2 £ ' I j 1 II i 9 E 9 S Figure 21. Water temperatures collected at " Donut Hole" and non- Donut Hole sites on Tule Lake National Wildlife Refuge, California, 1999. Box and whisker plots represent the median, 25- 75^ and 10- 90^ percentiles, and outliers. 29 do ( mgfl) I do ( mg/ l) OP> !• WKamm 01900 gGBM s ' S:' TP" » S i I ! if Figure 22. Dissolved oxygen concentrations at " Donut Hole" and non- Donut Hole sites on Tule Lake National Wildlife Refuge, California, 1999. Box and whisker plots represent the median, 25- 75 and 10- 90* percentiles, and outliers. 30 260.0 -. 240.0 220.0 - 200 0 180.0 => 160.0 H 140.0 - z 120.0 100.0 - 80.0 60.0 40.0 20.0 n n - » NT" —•— Depth ( m) fc= _ 6/ 2 107.00 0.8 Donut Hole Northwest - — .^^^ 6/ 7 77.20 0.8 H •—-^^ ' '—^ 6/ 14 25.30 0.8 6/ 21 24.80 0.8 - 1.0 o o O CJl depth ( m) 260.0 -, 240.0 220 0 200.0 180.0 - 2 160.0 z 140.0 - 120.0 100.0 - 80.0 - 60.0 40.0 20 0 0.0 » NTU — a— Depth ( m) , •=— mmm •= « a 6/ 22 44.00 0.9 Donut Hole West — « — — » - 6/ 28 26.60 08 •— 7/ 6 19.90 08 . ^ m — _ _ _ _ _ _ _ 7/ 13 25.70 0.8 • - _ — r- • 7/ 19 51.40 0.8 1.0 0.5 £ a. T3 0.0 260 0 240.0 - 220.0 - 200.0 - 180.0 i « n n _ H 140.0 - z 120 0 ^ 100.0 • 80 0 60.0 40.0 20.0 - u. u » NTU — m— Depth ( m) 6/ 22 93.70 0.8 6/ 28 95.40 0.7 Donut Hole East 7/ 6 72.70 0.7 7/ 13 32.30 0.7 —•'•"-""* 7/ 19 50.20 0.5 -"— 7/ 28 62.50 0.8 8/ 2 73.30 0.8 \ ^ 8/ 10 18.55 0.8 8/ 19 50.20 0.8 8/ 25 22.20 0.8 8/ 31 58.67 0.7 \ 9/ 8 14.38 0.8 9/ 14 11.03 0.8 9/ 20 7.00 0.7 9/ 29 7.80 0.7 j / A - 10/ 25 51.00 0.7 t - fT u 11/ 23 210.00 0.6 1 0 - 0.5 JZ jepi - 0.0 Figure 23. Turbidity at " Donut Hole" sites on Tule Lake National Wildlife Refuge, California, May to November 1999. 31 260.0 i 240.0 220.0 200.0 180.0 3 160.0 £ 140.0 - 120.0 100.0 80.0 60.0 40.0 20.0 0.0 » NTU —•— Depth ( m) • ^ 6/ 2 81.10 0.8 Donut Hole - — - ^ 6/ 7 49.20 0.8 — • 6/ 14 21.50 0.8 =— 1 6/ 21 24.80 0.8 r 1 0 o p d en depth ( m) 260 0 240.0 • 220.0 - 200.0 . 180.0 - K 160.0 • z 140.0 - 120.0 100.0 80.0 . 60.0 - 40.0 - 20.0 0.0 . t K » TII — a— Depth ( m) B — • 7/ 21 53.30 0.8 .— m-— 7/ 28 40.50 0.8 Donut Hole South _—• 8/ 2 56.80 0 9 » - ^ 8/ 10 17.13 0.9 —• 8/ 18 19.70 0 8 8/ 25 21.73 0.9 ^ \ 8/ 31 64.90 0.8 9/ 8 21.27 0.8 9/ 14 20.80 0.8 9/ 20 29.97 0.8 ^ - • - ^ 9/ 29 49.30 0.8 / / 10/ 25 33.70 0.8 / / 11/ 23 170.00 0.7 1 0 o o d en depth ( m) Figure 23 ( cont.). Turbidity at " Donut Hole" sites on Tule Lake National Wildlife Refuge, California, May- November, 1999. 32 260.0 -, 240.0 - 220.0 200.0 180.0 - 160.0 Z> 140.0 \ z 120.0 - z 100.0 80.0 60.0 40.0 20.0 - 0.0 _ NTU • depth ( m) y 5/ 26 12.30 0.7 6/ 2 58.70 0.8 A- 6/ 7 20.30 0.9 / / 6/ 21 57.40 0.8 // A A\\ 6/ 28 239.0C 0.8 V\ East Sump 1B J s in 81.70 0.7 : / I 7/ 12 10.40 1.0 \| A / \ J I s f 7/ 27 228.00 1.0 \ - V \ 8/ 2 88.00 0.8 8/ 10 40.00 0.9 8/ 18 38.17 0.8 8/ 31 11.30 0.7 9/ 9 7.00 0.7 9/ 14 6.17 0.7 9/ 20 5.83 0.7 • / 10/ 25 44.80 1.0 4-— \ ft . 11/ 23 186.00 0.5 1.0 ? e Q. 0.5 • 0.0 260.0 n 240.0 - 220.0 200.0 180.0 160.0 D 140.0 1— 120 0 z 100^ 0 80.0 60.0 An n 20.0 - 0.0 - —+— NTU —•— depth ( m) —•— 5/ 26 13.70 1.0 _, • —- « - 6/ 2 57.30 1.1 --•— ' \ 6/ 7 41.10 1.1 6/ 21 18.70 1.0 —•— / \ 6/ 28 138.0( 1.0 \ \ / ¥ West Sump 1B - . • — • / 7/ 7 ) 29.90 1.0 A \\ 7/ 12 88.90 1.0 k / \ / 7/ 27 19.00 0.9 / \ / \ 8/ 2 73.00 1.0 L \ \ 8/ 10 5.47 1.0 8/ 18 6.40 1.0 8/ 31 9.20 1.0 9/ 9 8.58 1.0 9/ 14 8.37 0.9 9/ 20 11.73 0.9 / / 10/ 25 39.50 0.7 f 11/ 23 85.00 0.8 1 5 sz Q. - 0 . 5 • - 0.0 260 0 240.0 220.0 - 200.0 - 180.0 160.0 3 140.0 t ; 120.0 100.0 80.0 - 60.0 An n . 20.0 0.0 » NT" — m— Depth ( m) 6/ 2 46.50 0.8 -~ « — 6/ 7 16.10 0.9 —•—. 6/ 14 39.00 0.8 / 6/ 22 9.71 0.8 English Channel Sump 1A 6/ 28 6.79 0.8 \ ^ _ 7/ 13 17.90 0.8 7/ 20 17.60 0.8 7/ 28 26.80 0.8 8/ 10 4.80 0.9 8/ 19 7.33 0.8 8/ 25 6.50 0.8 8/ 31 7.10 0.8 9/ 8 13.34 0.8 ==•== 9/ 20 15.50 0.8 J 9/ 29 22.60 0.7 — y / 10/ 25 98.70 0.8 11/ 23 146.00 0.8 1 5 - 1.0 — 0.5 - g 0.0 260 0 240.0 220 0 - 200.0 - 180.0 - 160.0 => 140.0 - £ 120.0 mnn . 60.0 40.0 - 20.0 u. u J •— NTU —•— Depth ( m) I 6/ 2 36.50 1.2 —•— 6 / 7 12.60 1.2 6/ 14 13.10 1.2 y 6/ 28 7.40 1.1 7/ 6 71.60 1.0 Northwest Sump 1A —•— 7/ 13 5.27 1.1 — » — —•— 7/ 19 28.50 1.1 7/ 28 20.50 1.2 8/ 2 32.10 1.2 ^- B—' 8/ 19 4.50 1.1 / 8/ 25 52.87 1.1 A ' \ 8/ 31 115.67 1.2 ="-•— \ —•=; 9/ 8 4.10 1.1 1 4- 9/ 14 7.89 1.1 —•— J I \ 9/ 20 12.43 1.1 — « ^ 10/ 25 180.00 1.1 11/ 23 164.00 0.9 1 S d jpth ( m) • 0.5 - o - 0.0 Figure 24. Turbidity at non- Donut Hole sites on Tule Lake National Wildlife Refuge, California, 1999. 33 Discussion Water Quality The area of the DH was delineated from plotted June through September locations of radio-marked suckers ( approximately 188 ha.). The location of the DH could also be seen as an area of relatively turbid water from aerial photographs from August 1998 ( Fig. 25) as well as aerial photographs taken in 1984. It is possible that the combination of 2 factors may cause the observed turbidity in the DH. First, seeps or springs may be present in the area which result in more favorable water quality during summer which attracts suckers as well as other fish species to the area. The resultant concentration offish ( suckers and chubs) may stir the sediments during feeding activities, thereby creating the observed turbidity. The additional turbidity in the DH may inhibit light penetration and the production of algae, thereby reducing photo synthetically elevated pH and the extreme minimum and maximums in DO typical of may water bodies in the Klamath Basin including Tule Lake ( Dileanis et al. 1996). The rise in turbidity at all sites in fall is likely due to the break down of rooted aquatic vegetation which then allows for wind induced wave action to stir the sediments. Other than the DH, all other sites had dense concentrations of rooted aquatic plants and/ or filamentous green algae during summer. June to September DO and pH dynamics in the DH appeared different than at NDH sites ( Figs. 20 and 22). The difference was greatest in early summer with the difference becoming smaller by late summer and essentially disappearing by fall. Whether this water quality difference was a result of the more turbid waters or inflow from springs is unknown. However, attempts by Service hydrologists to model inflows, evapotranspiration, and outflows from the sumps have resulted in a positive imbalance of approximately 21,000 acre- feet of water from April through September. This positive imbalance is greatest in spring and early summer, gradually lessening by summer and essentially disappearing by fall ( Tim Mayer, pers. comm.). If this inflow is occurring, it may explain differences in summer water quality between DH and NDH sites. June to September water quality in the DH may be critical to the over summer survival of suckers in Tule Lake as pH and DO in NDH sites during summer often exceeded the tolerance limits for the fish. DO and pH levels at DH sites were less variable and did not reach the extremes that were reached in NDH sites. The lowest DO measured during June through September at DH sites were 4.83 mg/ 1 ( DHWEST) and 4.96 mg/ 1 ( DHEAST). DO and pH during summer from this study were similar to values collected by Reclamation in 1992 ( Table 3). Buettner and Scoppettone ( 1990) found juvenile suckers only where DO was above 4.5 mg/ 1. It is currently believed that adult suckers become stressed at DO levels below 4.0 mg/ 1 with mortality occurring at or below 2.0 mg/ 1 ( M. Buettner, pers. comm.). The relatively high over- summer survival of radio- marked suckers, compared to suckers radio- marked in Upper Klamath Lake ( M. Buettner, pers. comm), is further evidence of suitable summer water quality conditions in the DH on Tule Lake. 34 Figure 25. " Donut Hole" in Sump 1( A) of Tule Lake NWR. Note visible turbidity of area. 35 Table 3. Mean dissolved oxygen, pH, conductivity, and temperature on Tule Lake National Wildlife Refuge, California, July and August 1992. Data are from 2 sites; 1 site each in Sump 1( A) ( within the ADonut Hole@) and 1( B). All data were from 96 hour continuous readings from Hydrolabs. Data were collected at intervals of 1- 2 hours. ( Data summarized from U. S. Bureau of Reclamation). Site Sump 1( A) Sump ( IB) Depth ( M) < 0.5 0.51- 1.5 > 1.5 < 0.5 0.51- 1.5 > 1.5 pH (± SD) ( 1200- 1700 hrs) 9.32 ± 0.83 n= 81 9.22 ± 0.93 n= 26 8.30 ± 0.71 n= 10 9.65 + 0.44 n= 21 9.79 ± 0.45 n= 7 No data Temp ° C (± SD) ( 1200- 1700 hrs) 21.85 ± 2.84 n= 81 21.53 ± 2.46 n= 26 19.90 ± 1.59 n= 10 22.96+ 1.10 n= 21 22.11 ± 0.51 n= 7 No data Conductivity 500 ± 266 n= 81 598 ± 277 n= 26 859 ± 694 628 ± 148 n= 21 571 ± 74 n= 7 No data DO1 Oof 31 days - - 8 of 21 days - - 1 Proportion of monitored days having a minimum dissolved oxygen level below 5 mg/ 1. ( Data from U. S. Bureau of Reclamation) pH levels in the DH generally remained below 10.0 whereas non DH sites frequently exceeded 10.0 ( Fig. 19). Falter and Cech ( 1991) determined a maximum pH tolerance in shortnose suckers of 9.55+ 0.43 under laboratory conditions, levels generally exceeded in June - September at non DH sites and some DH sites in late summer. Buettner and Scoppettone ( 1990) found juvenile fish in Upper Klamath Lake largely at sites with pH < 9.0, as did Simon et al. ( 1996) in 1994. However, in 1995, Simon et al. ( 1996) found that most juvenile fish ( 54%) were captured in areas of higher pH (> 10.0). Laboratory studies indicate significant mortality of larval and juvenile fish at high pH values (> 9.55) ( Falter and Cech 1991) and 9.92- 10.46 ( Bellerud and Saiki 1995). Previous water quality and fish health studies on the refuge determined that water quality conditions were stressful to aquatic life and was resulting in a high ( up to 37%) proportion offish with deformities ( Dileanis et al. 1996), however, studies of sucker ecology in Tule Lake have indicated that individual fish in the lake have a high condition factor and are free of external parasites ( Scoppettone and Buettner 1995). Bennet ( 1994) recognized this apparent inconsistency, stating, A... the observation that Tule Lake suckers are in better physical condition than Upper Klamath Lake suckers indicates that certain areas of the aquatic system may be of particular importance for the recovery of those species. ® In the case of Tule Lake this Acertain area@ is likely the DH.. Suckers in Tule Lake may be in good condition because of their limited population size, the abundant food resources in this lake, and adequate water quality ( in the DH) to survive the summer period. 36 Sucker movements Although, suckers were relatively sedentary during most periods of the year, they exhibited the ability to make long distance moves in relatively short periods of time, particularly during the April spawning period. The northwest corner of Sump 1( A) receives about 90% of the inflow from the Lost River and spring winds on Tule Lake tend to move large quantities of water through the AEnglish Channels back and forth between Sump 1( A) and 1( B). This movement of water at both locations may explain the movement of fish observed in April and May. Suckers may be attracted to both locations when seeking spawning habitat in spring. Recruitment During the April marking period, most captured suckers appeared to be physiologically ready to spawn; however, only one fish moved into the river. Of 10 radio- marked fish monitored by Reclamation in 1993- 95 no fish attempted to run the Lost River. This low proportion offish that attempt to spawn may have one or several causes or a combination, including: 1. Stress of handling and implanting radio- transmitters so close to the spawning season may prevent fish from becoming reproductively active. 2. Under normal conditions, only a small proportion of Tule Lake suckers may attempt to spawn in any particular year. 3. Flow conditions in or at the mouth of the Lost River may be inadequate to draw the fish into the river. 4. A shallow bar (< 0.3 m) of deposited silt exists between the lake and the mouth of the river which may form a physical barrier to the fish. At the present time, a mandated flow of 30 cfs is released below Anderson- Rose Dam to provide spawning habitat at the Dam. Although this flow is intended to provide suitable spawning conditions at the Dam, these flows may be inadequate to entice fish into the river. It is likely that the historic spring flows in the Lost River were many times higher than current regulated flows. However, given that the fish are largely unsuccessful in spawning and risk additional mortality traversing the river, adult survival may be enhanced by remaining in the lake. Scoppettone and Buettner ( 1995) also observed no radio- marked fish from Clear Lake to move into Willow Creek during the spring spawning period. In this case the authors attributed this result to either capture stress or low stream flows during spring. 37 Habitat use Although the DH is relatively shallow relative to other areas of Tule Lake, use of the DH may be mandatory to ensure over- summer survival. Although deeper waters are available to the fish, especially in the northwest corner of Sump 1( A), DO levels, in particular, likely preclude their use. Suckers did not move out of the DH until October when DO levels began to rise with cooler water temperatures. Although, Sump 1( B) contained suitable water depths and water quality conditions in fall, no suckers were located in this area. It is possible that suckers may prefer not to pass through the pipes connecting the Sumps or the proximity and flow from the Lost River in the northwest corner of Sump 1( A) may make this area more attractive as an over- winter habitat area. The relative lack of water depth in the DH as well as other areas of the sumps is becoming of increasing concern because of the loss of water depth through sedimentation. If suckers require a minimum of 3 ft of water, as is current believed ( M. Buettner, pers. comm.), current rates of sedimentation in the sumps threaten the future suitability of Tule Lake for suckers. Based on a comparison of bathymetric surveys conducted by Reclamation in 1958 and again in 1986, sedimentation has been steadily reducing the water holding capacity of both sumps. Between the 1958 and 1986 surveys ( 28 years), Sump 1( A) has lost 22.4% of its water capacity and Sump 1( B) has lost 30.8% of its capacity due to sedimentation. This would indicate a total mean sedimentation of 11.8 inches over this time period ( U. S. Bureau of Reclamation, unpubl. rep). Over the last several years, an attempt has been made to store additional water in Tule Lake during summer by raising water levels above 4034.60 ft. This increase in water elevations ( between 4034.60 and 4034.90 ft) has somewhat mitigated the loss of depth through sedimentation. However, without reinforcing and raising the levees around the sumps, there is a limit as to how high water elevations can rise. At elevation 4035.50 ft., operating regulations require breaching the sumps into overflow areas ( Sump 2 or 3). Although increased summer operating levels may assist the fish, they may also increase the risk of a flood event requiring the breaching of the sumps with potentially negative impacts to the fish. Acknowledgements The authors are indebted to fisheries biologist from the U. S. Bureau of Reclamation, Klamath Project, especially M. Buettner, B. Peck, and M. Green whom provided and surgically implanted radio transmitters, captured adult suckers, located fish from fixed wing aircraft, and assisted with study design. K. Miller from Klamath Basin National Wildlife Refuge collected telemetry, water quality, and GPS data and ensured all data were collected and coordinated consistent with study design. T. Mayer provide training in the calibration, deployment, and downloading of data from the hydrolabs and assisted with interpretation of water quality data. 38 Personnel Communications Buettner, M., Fisheries Biologist, U. S. Bureau of Reclamation, Klamath Project Office, 6600 Washburn Way, Klamath Falls, Oregon. Mayer, T., Hydrologist, U. S. Fish and Wildlife Service, Portland Regional Office, Lloyd Center, Portland, Oregon. Literature Cited Bellerud, B., and M. K. Saiki. 1995. Tolerance of larval and juvenile Lost River and shortnose suckers to high ph, ammonia concentration, and temperature, and to low dissolved oxygen concentration, National Biological Service, California Pacific Science Center, Dixon 103pp. Bennett, J. K. 1994. Bioassessment of irrigation drain water effects on aquatic resources in the Klamath Basin of California and Oregon. Ph. D Dissertation. University of Washington, Seattle. 197pp. Buettner, M. E., and G. Scoppettone. 1990. Life history and status of catostomids in Upper Klamath Lake, Oregon. National Fisheries Research Center, Reno Field Station, Reno, Nevada, 108pp. Coots, M. 1965. Occurrences of the Lost River sucker, Deltistes luxatus ( Cope), and shortnose sucker, Chasmistes brevirostris ( Cope), in Northern California. Calif. Fish and Game 51: 68- 73. Dileanis, P. D., S. K. Schwarzbach, and J. K. Bennett. 1996. Detailed study of water quality, bottom sediment, and biota associated with irrigation drainage in the Klamath Basin, California and Oregon, 1990- 92. U. S. Geological Survey, Water- Resources Investigations Report 95- 4232, 68pp. Falter, M. A., and J. J. Cech. 1991. Maximum pH tolerance of three Klamath Basin fishes. Copia 4: 1109- 1 111. Simon, D. C, G. R. Hoff, D. J. Logan, and D. F. Markle. 1996. Larval and juvenile ecology of Upper Klamath Lake suckers. Annual Report: 1995, Department of Fisheries and Wildlife, Oregon State Univ., Corvallis. 60pp. 39 Scoppettone, G. G., and M. E. Buettner. 1995. Information on population dynamics and life history of shortnose suckers ( Chasmistes brevirostris) and Lost River suckers ( Deltistes luxatus) in Tule and Clear Lakes. U. S. Geological Survey, Reno Field Station, Reno, Nevada. 79pp. U. S. Bureau of Reclamation. 1998. Lost River and shortnose sucker spawning in Lower Lost River, Oregon, U. S. Bureau of Reclamation, Klamath Falls, Oregon. 1 lpp. . 1993. Lost River { Deltistes luxatus) and shortnose { Chasmistes brevirostris) Sucker Recovery Plan. Portland, Oregon 108pp. Hydrolab Corporation. 1997. DataSondeR 4 and MiniSondeR water quality multiprobes, users manual. Hydrolab Corp., Austin, Texas. Title: Ecology of shortnose and Lost River suckers in Tule Lake National Wildlife Refuge, California : progress report, April - November 1999 Author: Hicks, Lisa A.; Mauser, David M.; Beckstrand, John; Thomson, Dani Year: 2000, 2005 Ecology of shortnose and Lost River suckers in Tule Lake National Wildlife Refuge, California, Progress Report, April - November 1999 Lisa A. Hicks, U. S. Fish and Wildlife Service, Klamath Basin National Wildlife Refuge, Route 1, Box 74, Tulelake, CA 96134 David M. Mauser, U. S. Fish and Wildlife Service, Klamath Basin National Wildlife Refuge, Route 1, Box 74, Tulelake, CA 96134 John Beckstrand, U. S. Fish and Wildlife Service, Klamath Basin National Wildlife Refuge, Route 1, Box 74, Tulelake, CA 96134 Dani Thomson, U. S. Fish and Wildlife Service, Klamath Basin National Wildlife Refuge, Route 1, Box 74, Tulelake, CA 96134 Introduction The Lost River ( Deltistes luxatus) and shortnose ( Chasmistes brevirostris) suckers were federally listed as endangered species on July 18, 1988 ( Federal Register 53: 27130- 27134). Both sucker species are relatively long- lived, have a limited geographic range, and are endemic to the Upper Klamath Basin of Northern California and Southern Oregon. Habitat degradation from water diversions and loss of riparian and wetlands habitats associated with agricultural development within their historic range is believed to be the major reason for the species decline ( U. S. Fish and Wildlife Service 1993). A more detailed description on the life history, habitat requirements, and causes of decline of the species can be found in the Lost River and Shortnose Sucker Recovery Plan ( U. S. Fish and Wildlife Service 1993). Tule Lake National Wildlife Refuge ( NWR), established in 1928, consists of 2 return flow sumps ( Sump 1( A) and 1( B)) totaling 13,000 acres surrounded by 17,000 acres of intensively farmed lands ( Fig. 1). The refuge and surrounding private agricultural lands occupy the historic lake bed of Tule Lake, a 95,000 acre lake and marsh area that was reclaimed in the early 1900fs as part of the Klamath Reclamation Project. Current management of the refuge is directed by the Kuchel Act of 1964 which mandates the refuge be managed for the major purpose of waterfowl management but with optimal agricultural use that is consistent therewith. Both sumps are shallow ( 0.1 - 2.0 m) and consist of approximately 10,500 acres of open water with a 2,500 acre shallow (< 0.1 m) emergent marsh at the northeast corner of Sump 1( A). Tule Lake has been identified as a potential refugia for both sucker species ( U. S. Fish and Wildlife Service 1993). Tule T like National Wildlife Sump 3 Lease lands Field . Station Cocbetative Fanning Fields Area J Lease Lands Sump 2 I ease I , ands Figure 1. Tule Lake National Wildlife Refuge, California. During winter, water within the sumps is comprised primarily of local runoff and during summer water is comprised primarily of irrigation return flows, originating from Upper Klamath Lake. Summer water quality in the sumps is similar to other water bodies within the Upper Klamath Basin and is considered hypereutrophic ( Dileanis et al. 1996). Water quality problems include low dissolved oxygen ( DO) and high hydrogen ion concentrations ( pH) and unionized ammonia. Water quality in the Tule Lake sumps is directly affected by hypereutrophic conditions in Upper Klamath Lake ( U. S. Fish and Wildlife Service 1993). Studies conducted after publication of the Shortnose and Lost River Sucker Recovery Plan indicate that Tule Lake contains an estimated 159 ( 95% CI = 48- 289) shortnose and 105 ( 95% CI = 25- 175) Lost River suckers ( Scoppetone and Buettner 1995). Confidence intervals for these estimates are large because of small sample sizes and low rates of recapture. Recruitment rates for the Tule Lake population via spawning below Anderson- Rose Dam is low with significant larval production occurring only in 1995 ( monitoring occurred 1991- 99) ( M. Buettner, pers. comm). Entrainment from the irrigation system is likely the largest source offish for Tule Lake ( U. S. Bureau of Reclamation 1998). Both species of suckers in Tule lake are in good physical condition relative to fish in Clear Lake and Upper Klamath Lake with Tule Lake fish being generally heavier and exhibiting few if any problems with parasites or lamprey. ( Scoppetone and Buettner 1995). U. S. Bureau of Reclamation ( Reclamation) biologists tracked 10 radio- marked suckers in Tule Lake from 1993- 95. From these studies, specific use areas by time period were identified with over 99% of radio locations occurring in Sump 1( A). Of particular importance from these studies was identification of an over- summer site in the south central region of Sump 1( A) termed the ADonut Hole# ( DH). In early 1999, the U. S. Fish and Wildlife Service ( Service) proposed a wetland enhancement project on the 3,500 acre Sump 1( B). The project was designed to improve habitat for waterfowl and other associated wetland species as well as improve water quality through the conversion of Sump 1( B) from an open body of shallow water to an emergent year- round flooded wetland. The primary mechanism to create the desired habitat condition is a series of annual spring/ summer drawdowns thereby creating conditions suitable for germination of desired emergent plant species. Of principal concern in developing the project was the potential effects on suckers within the sumps. Because of the proximity of both sucker species in adjacent Sump 1( A), a project monitoring plan was developed to ascertain the potential effects of the Sump 1( B) Project on suckers and water quality. Our monitoring design benefitted from studies of water quality and sucker movements by Reclamation biologists from 1992- 95. This report summarizes findings of the first year= s pre- project monitoring effort ( April- December, 1999) relative to water quality and movements of radio- marked suckers. Objectives 1. Describe seasonal distribution and movement patterns of both sucker species in Tule Lake NWR and determine if fish movements have changed since initial studies by Reclamation biologists in 1993- 95. 2. Characterize water quality, in space and time, of areas used by adult suckers compared to areas which are not used. 3. Document and describe movements of radio- marked suckers to spawning areas below Anderson- Rose dam. 4. Determine whether recruitment of larvae and juvenile was occurring below Anderson- Rose Dam. Methods Monitoring radio- marked adult suckers In April and May, 1999, Reclamation biologists captured 14 suckers and surgically implanted radio- transmitters ( ATS, Isanti, MN) having a projected battery life of 12 months. Each transmitter had an external antennae that exited the body cavity near the lateral line of the fish. Eleven Lost River and 3 shortnose suckers were captured using trammel nets at the northwest corner of Sump 1( A) ( 9 fish) and immediately downstream of Anderson- Rose Dam on the Lost River ( 5 fish) ( Table 1). We located radio- marked fish via air thrust boats using a scanning receiver and 4- element yagi antennae. Fish were located fish 4 times/ month during March and April, 2 times/ month from May through September, and once per month from October through December. Fish not located via boat were located from fixed wing aircraft. We determined fish locations by moving as close as possible to undisturbed fish and recording locations with a Global Positioning System ( GPS). All GPS positions consisted of 180 rover points/ location and were differentially corrected via post processing software ( PFinder ver. 2.11). We recorded depth information at each fish location. To determine timing and duration of the spawning migration, we monitored radio-marked fish from vehicles on the east levee of the Lost River downstream of Anderson- Rose Dam. Table 1. Data from Lost River and shortnose suckers captured on Tule Lake National Wildlife Refuge, California and Anderson- Rose Dam, Oregon in 1999. RADIO TAG 165.043 165.063 165.073 165.103 165.084 165.094 164.641 164.863 164.494 164.854 165.054 164.845 164.763 164.914 CAPTURE DATE 4/ 2/ 99 4/ 2/ 99 4/ 2/ 99 4/ 2/ 99 4/ 2/ 99 4/ 2/ 99 4/ 9/ 99 4/ 2/ 99 4/ 9/ 99 4/ 30/ 99 5/ 5/ 99 5/ 5/ 99 5/ 18/ 99 5/ 18/ 99 CAPTURE LOCATION TULELAKE SUMP1A TULELAKE SUMP 1A TULELAKE SUMP 1A TULELAKE SUMP 1A TULELAKE SUMP1A TULELAKE SUMP 1A TULELAKE SUMP1A TULELAKE SUMP1A TULELAKE SUMP 1A ANDERSON ROSE DAM ANDERSON ROSE DAM ANDERSON ROSE DAM ANDERSON ROSE DAM ANDERSON ROSE DAM SPECIES LOST RIVER LOST RIVER LOST RIVER SHORTNOSE SHORTNOSE LOST RIVER SHORTNOSE LOST RIVER LOST RIVER LOST RIVER LOST RIVER LOST RIVER LOST RIVER LOST RIVER SEX FEMALE FEMALE FEMALE MALE FEMALE FEMALE FEMALE MALE FEMALE FEMALE MALE MALE MALE FEMALE WEIGHT NO DATA NO DATA NO DATA NO DATA NO DATA NO DATA 2830 g 1040 g 5260 g NO DATA 2214 g 1542g 2350 g 1811 g FORK LENGTH 777 mm 681 mm 754 mm 473 mm 523 mm 754 mm 544 mm 440 mm 775 mm 753 mm 556 mm 486 mm 594 mm 477 mm PIT TAG NO. 1F3E34432C 1F39064959 1F4C5A6754 1F07315752 1F31462743 1F4C5A6754 1F3726750F 1F36490062 1F37103466 1F390F1801 1F3E2A7702 1F36443235 1F30753309 1F390E6B2F Recruitment Reclamation biologists conducted larval and juvenile sucker surveys during May and June by sampling, visually and with dip nets, the emergent vegetation at the periphery of the Lost River downstream of Anderson- Rose Dam. Egg viability surveys were conducted in the gravel sediments immediately below the dam in May. Water quality We preselected water quality sampling sites ( Fig. 2, Table 2) in Sump 1( A) to correspond to adult sucker use areas as determined by studies of radio- marked adult suckers conducted by Reclamation in 1993- 95 ( Fig. 3). We selected 2 sites in Sump 1( B) which met or exceeded the minimum depth requirement (> 3ft) for both sucker species ( M. Buettner, pers. comm.) after referring to 1986 bathymetric maps. We attempted to obtain data from each site twice/ month. We moved 2 sample sites ( Donut Hole and Donut Hole Northwest) early in the summer and 1 site ( Donut Hole West) ( Fig. 2) during mid- summer to better represent summer use locations of radio- marked fish. From May through November, we measured water quality parameters ( dissolved oxygen ( DO), hydrogen ion concentration ( pH), and temperature (° C)) using DataSonde 3, 4 and 4a= s ( Hydrolab Corp., Austin, Texas) ( hereafter referred to as Hydrolabs) 26 cm ( 12 in) above the sediment. We suspended Hydrolabs, within PVC tubes, from metal fence posts driven into the sediment. Data were collected hourly over a 96 hr period at each monitoring site. We downloaded data from Hydrolabs using the Hyperterminal software package v. 690170 to a personal computer. Unit probes were cleaned and calibrated according to Hydrolab guidelines ( Hydrolab Corporation 1997) and local geographic standards. Using the same deployment schedule as with our Hydrolabs, we sampled turbidity at each site using a Portable Turbidimeter model 21 OOP ( Hach Corp., P. O. Box 389, Loveland, CO 80539). We collected water samples 27 cm ( 12 in) above the sediment at each sample site. We measured turbidity in NTUs, following the guidelines in the product manual and we measured water depth using a hand- crafted wooden pole, marked in measured increments. We summarized water quality data using Microsoft 8 EXCEL software v. 97 SR- 1 and SPSS for Windows release 9.0.0. Because of the apparent difference in summer water quality in the DH versus other sampling sites, data were summarized as DH sites and Non- DH ( NDH) sites. Tule Lake NWR Water Quality Monitoring 1999 MfSVTHOLE \ OKTIIH ' w Background Hvdrolon> Luke m Mudflats Uplands X Water Vionitonny Stations ( Hydrolafa sites) MK ker Radio \ ckmcin L. Hicks. D. .1 Beckitraod, K Miller, USFWS Background HydfOlOf} Sat'I Wetlands Invcnlon LSI Sh S Map Projection UTMZCM IO, WGS- 4 By: L. Hkks. USFWSUSBR 02/ 00 i Figure 2. Water quality sample sites, Tule Lake National Wildlife Refuge, California, 1999. 8 Table 2. Characteristics of water quality sampling sites, Tule Lake National Wildlife Refuge, Tulelake, California, 1999. SITE NAME NORTHWEST SUMP 1A DONUT HOLE NORTHWEST DONUT HOLE WEST DONUT HOLE SOUTH DONUT HOLE DONUT HOLE EAST ENGLISH CHANNEL WEST SUMP IB EAST SUMP IB PUMP 10 SUMP 1A2 SITE ABBREVIATION NWS1A DHNWSlAor DHNW DHWEST DHSOUTH DHSlAorDH DHEAST ECSlAorEC WS1B ES1B PMP10 UTM N 4642199 4638316 4638881 4638144 4637299 4639024 4634604 4634153 4633948 4636635 UTME 620803 620542 321022 621355 621475 621971 625041 636647 628835 624748 DEPTH of MONITORING SITE ( m) 1 1.2 0.9 0.9 0.8 0.7 0.8 0.8 1.0 0.8 0.5 1 Depth of water at deployment 2 Pump 10 data will not be discussed in this document. Results Radio- marked suckers We located fish 231 times in locations similar to those determined by Reclamation biologists in 1993- 95 ( Figs 3- 4). Lost River and shortnose suckers did not appear to differentiate use of the sump by species; we located both species intermixed throughout the monitoring period. With the exception DH and DHNW ( Fig. 2), water quality sampling sites were close to seasonal sucker use areas. Of 14 suckers marked, mortality occurred in only 1 fish. A Lost River sucker (# X9) was tagged on 18 May at the Anderson Rose Dam; she was not located again until 23 days later on 9 June. From 9 June to 17 November, # X9 was located by signal within approximately 15 m of the original location based on the location data. It is likely that this fish died in early June within 2- 3 weeks of being radio- marked. It is unknown if this mortality was related to the stress of handling and marking or some other cause. April - May - In April- May, a period of maximum fish movements ( Figs. 5- 18), most suckers congregated in the AEnglish Channel ® between the sumps with a scattering offish located between the northwest corner of Sump 1( A) and the AEnglish Channel ® ( Fig. 4). Only 1 fish radio- marked in Tule Lake moved into the Lost River. This particular fish, a female shortnose sucker (# G9) was radio- marked in the northwest corner of Tule Lake on 9 April, was located in the AEnglish Channel ® on 14 April, and subsequently was located in Lost River below Anderson Rose Dam on 29 April and 6 May. Tule Lake Sucker Radio Telemetry \ pril 1993 - \! a> 1995 Hi tckwtstmd H) drohgy mm Marth/ Wi'lhiml • • River I Sucker Locations o Jan - Mar & Apr - May ° Jim - Sep • O t t - l h i 1 I . . . . . . ydtOl Ig) -: i '•'•, l: i M h - c .1 J I SI WS UtoBiihywwUy KkmrtiiB ••. iraOffia MapPinoiccii.- i rM2oni VM, S- » 4 • HJ I-. IKKV USffW& n SBB Figure 3. Locations of radio- marked suckers from studies conducted by U. S. Bureau of Reclamation, on Tule Lake National Wildlife Refuge, California, 1993- 1995. 10 Tule Lake NWR Sucker Radio Telemetry April - December 1999 Oregon California [ Sump 1A Background Hydrology J Lake Uplands SOcker Locations • Apr May o Jun - Sep • Oc! - Dec \| Qanuthole area = * 466 acres ( manually est from fish bca Suckei EUdiQ Tdctrcter: L Hi cks, D TtccnsDn, : Nati Wedatd^ Inventory. USTWS i t Hi cfa, usFwsnrsBH o 2/ 00 Figure 4. Locations of radio- marked suckers on Tule Lake National Wildlife Refuge, California, 1999. 11 Tule Lake- Sucker Radio Telemetr> - 1999 MMti « phrnl Fish: Lost River Sucker " A9" Sex Female Length: 777 mm fag I ocation I ulc I ; ike Sump IA Tai: Dare: 04/ 02 99 Vlort. Date: 3 - O 5 ni 0 5 - 1 ni ( Surface Fixation - 4034.9( 1') Lain' ihpth 1 - 15m Itydrolah tUm » t tm fcdarl .' i rein: l. llni. i. Becb- rmc l^ . I M I ^ I V I M . Kl; nn: nli limm Xvtup,- :, rr, k, I M •'• - \ * e BMb% « ldry KIWWHI I t em ,^ wnOi-... I SB I Background Hy* » : 4.. .. , „ \| WCIIWKIJ faivewior^. I'SI A S >• • ••• i •• i MZcne IC ' •..-• .: i;% i n . , i s , u s Figure 5. Movements of radio- marked sucker A9 on Tule Lake National Wildlife Refuge, California, 1999. 12 Tule Lake- Sucker Radio Telemetry ~- 1999 Hsh ], ost River Sucker"! Sc\ Female Length: UK] mm Tag Location [ We Lake Sump IA IML Dace U4/ O? W Mort Date: • i Khrr( m » depth) • 1 Mwrvl. Will. 1.1,1 I \|- l Muil I t * 3 - O 5 m 0 5 - t rn ( Surtax i: Nation - 4O34. W) flyJrttlaff SiKker RacfcTclemdn: I. IliduU. Bccks CompK. i BFW8 I. a.- Mil ,. l klmulklfaun \ « » OI.. . I MM Background llyfrotogv \ « bonB\| W ctlands inv « « or., U8FWS Map IVv^ vi ... i M ,. !• ' ••"• . I:-. \| \|\| ... i JFWS Figure 6. Movements of radio- marked sucker B9 on Tule Lake National Wildlife Refuge, California, 1999. 13 Tule Lake- Sucker Radio Telemetry - 1999 Fidi Lost River Sucker * C9" Sex Male Length: 619 mm Tag Location I ule Lake Sump IA Fag Date: M/ 02 w VIon. Date: { Surface Fixation - 4II34. W) tiat- ttffawmf th- frohf(\ • • Khii i> nJv\|> th) H i \ iM, vh\ wtl,..., i UplniKi Lak mm MU. I n. i 3 - 0 5 ni 0 5 - 1 ru • I n kaAo Tckwdn: LHkfcaJ. Beduimd P HMUWM K V'l « • .\|: I- II: I-\| I I n i ii Cwnpk. I 8FWS Klmwil.[ ten< •• . : M . . . I M : mind I l > * o t i c \ Ntttaaal Wetlands Inventory* I ^\| •.!•••• • • . • I -. I \ \| . , K 1 1 . i •• » •• -; !:•• I II . I SFWS r Mil . Figure 7. Movements of radio- marked sucker C9 on Tule Lake National Wildlife Refuge, California, 1999. 14 Tule Lake- Sucker Radio Telemetry - 1999 Haf kgnm n BB Rh « ' i MM. Fish Shortnose Sucker " l) l>" Sex Male Length: 473 nun ail Location: I ale Lake Sump IA Tag Date 04/ 02/ 99 Mort. Date: I Surface Fixation - 41> 34. lW) /....'.:• Depth Mi, I lbtx 0- OSm ^ ^ 0 5 - 1 rti - I - ' I •' • • ' ' • I HkfcU. lUbrxilHil) I ! . . . ! - . K Mil M KlttiHtfiBttk K « Aig « : . , - , - , L . I M ''. •• Ifydrolah Kit,-* i., i.- . il ... (.. , , , i , , •. . ; „ , . . , M ! - U a d ^ r t w n d ! ! > * • ••'• • t n \| XVctinjKlt [ mcTrt « . T\. • SFWS I • • . . • • , , • l:% \| n ...... i M A S * £> Figure 8. Movements of radio- marked sucker D9 on Tule Lake National Wildlife Refuge, California, 1999. 15 Tule Lake- Sucker Radio Telemetry - 1999 Fish Shortnose Sucker T39" Sc\ Female Length: 523 mm rag Location I ule I ake Sump IA rag Date M/ 02 w Date: • 1.1 I i) I 1-.. 1 • \| i i . . I. llcct. M m i l l ) ] Compl- • ' " I '• S 5> NJUOIWI Wetlands b i v c m u r y I IS I » S • ••• I " I ••. l/. nc It. i . . . : - . , ' II-. \| \|\| ..... Figure 9. Movements of radio- marked sucker E9 on Tule Lake National Wildlife Refuge, California, 1999. 16 Tule Lake- Sucker Radio Telemetry - 1999 Fish Lost River Sucker " IV Sc\ female Length: 754 mm Tag Location Tule Lake Sump 1A * rag Date 040; 99 Vkirt Date: ( Surface Fixation - 4( 134.90') Hat ground Hydrology U • : • • Rhtr< iM » < Jvpfh) • iM.., lll » r • i M. tvh\ VHl,, na 0.0,5m Uphml » 0S- 1rt. 1 - 1 5 IT » 1 £ m fackcrRadk> 1 r .. In: UfisfcaJ. Ikvkwjjjui P » •, K V, 1 • l: m: rli M a Jfcflifc* CorapUv I IFWS Uydrolth sit,- s i , i t \ t, il> m. f n Klmwlh tfewn .\ wn < » flfa . I SBR K o t o ^ : \ ai,,, na\| Wctljmd bivcm^ f • I SFWS Map hV^ vl .. . I MZpftClO Cony aid I;-, i n , . UWTOS Figure 10. Movements of radio- marked sucker F9 on Tule Lake National Wildlife Refuge, California, 1999. 17 Tule Lake- Sucker Radio Telemetry - 1999 Fish Shortnose Sucker " Q9" I cm ale Length: 544mm I. IL1 Location Tule Lake Sump IA * rag Date 04/ 09/ 99 Mori ( Surface rloaliun - I II . . I. \'-.-\-- m.' I-K V i ! l • l : n i : r l l ! - i i : ii : . r , : . \| , . I s\|\ VS KlmuHi Btom Aivs 4 M1K. I SBR \ j i > i m l Wetlands invcnlon i 5FWS M. « ;. ' - . . I - . I M / . „ . • \| » . I II , • I SFWS BB Ki^ i imi M \ hrvh\\ ilhiml Upland Lais Otfttk MuiJ Hals Figure 11. Movements of radio- marked sucker G9 on Tule Lake National Wildlife Refuge, California, 1999. 18 Tule Lake- Sucker Radio Telemetry ~ 1999 • Jit" Fish Sex Length: Tag Location: Tag Date: Sh oi1no so Male 440 mm Tule 1 < ikc 04/ 09/ 99 / Sucker Sump " H9" IA f tif( rtitiini / / i Kh< < 1- 1 . ri. l Mud FliitK 0 - 0 5 m 05 - 1 ni < SurfiKi 1 , - > 18m K V , , • l; , - n : , l , 5 , , , : . • „ • , '• • ' • • : ' k • ' s \| ' ' ' s K i i. l I-. . . . tVu. I M i ^ ' ^ \ tbonn\ Wetl « nd « faiv « mor>. I . \ I A • » - i I M „, \| i. Ih \| \|\| , , I M Figure 12. Movements of radio- marked sucker H9 on Tule Lake National Wildlife Refuge, California, 1999. 19 Tule Lake- Sucker Radio Telemetry - 1999 I- isii Lost River Sucker " 1 Sc\ Female Length: 775 mm Tag Location: Tule Lake Sump IA Tag Dale: 04/ 09/ 99 Mort. Date: ( Surface I* k^ atinn Tckmrtn: l.\|\| uk. I. K J y me l> I..: II> M K •-.•. I - I : . . , : Compkv • BPWS "' ••' Klmwlbl? ti » m A* MOffice I SBR IvckuioRv : \ atxin » l Wetlands biv « Mory. I > I / i < n k j f M U U l f i x • • • ' < • . • • Khri ( IM » tlr\|> rh) Mat vh Wit I HI ii I LpbmJ Figure 13. Movements of radio- marked sucker 19 on Tule Lake National Wildlife Refuge, California, 1999. 20 Tule Lake- Sucker Radio Telemetry - 1999 Fish: I- osi River Sucker " P9" Sc\ Female Length: 7^ ' m m lag Location Anderson Rose Dam Tag Dale: 04/ 30/ 99 Mort. Date: ( Surface bk'talkm - 4UJ4. W) % mkm i .' i eraetn: \|.\| ikk* J. lkvl> « uui I) . . . . i - K '•.'. . - i . . r . . i . BMte Rvtug « , « ., .. . . - . M V . . Compk. i IPWa I « l.- . ll ,. t ,.. , , , \| , , •. . „ ,. . \| M i • E* K* gr° umi I K v H , ^ htaHml Wctl » nd » knvMori i -- I - s ^ • •• I •• I M i . , - It. > •—•• . i;-. i II . . i MWN Figure 14. Movements of radio- marked sucker P9 on Tule Lake National Wildlife Refuge, California, 1999. 21 Tule Lake- Sucker Radio Telemetry - 1999 Fish Lost River Sucker " i;(>" Sex Male Length: 556mm Tag Location Anderson Rose Dam Tag Date 05 05 w Mort. Date: ( Surface H o at ion - - MM4. W) • i • i n. t . i. ikJ^•. m..- I) . M. HV. K Vi . • hnrnflh ii » m Hvfil^- '" I - I K ••. . I" K i r •• . M ... I MiM \-, ..,.•. \ , ,,.\| v. , \|,,.\|. ( r. v : , f . l MH • . ! ., I M „ \|. Figure 15. Movements of radio- marked sucker U9 on Tule Lake National Wildlife Refuge, California, 1999. 22 Tule Lake- Sucker Radio Telemetry - 1999 Fish: Lost River Sucker " W Sox: Male Leagth 486 mm \ AII Location; Anderson Rose Dam Tag Date: 05/ 05/ 99 Mort. Date: ( SurfiK- c Floaiiun 4 « . U. W\| •• ' • •• ' • ; • ' ' ' ' I I I . . • 1. Bedu HI.- D . K V I " , I . < l: iMi; iTh : - i • : .1 MIK! KI. HH I - • • > • . • • \ 1 i i i v . v l . r i l - i r . v : • ! • . 1 • . . . 1 . • 1 \ \| , , c 1. Figure 16. Movements of radio- marked sucker V9 on Tule Lake National Wildlife Refuge, California, 1999. 23 Tule Lake- Sucker Radio Telemetrv - 1999 Fish: Lost River Sticker " W(>" Sex: Male Length 594 nun I nil Location: Anderson Rose Dam Tag Date: 05/ 18/ 99 Meet. Date ( Surface H o at inn 4< i. U/) i » ') - ' • ' I ' : ' - ' • I Hid • i. Bcvl. v.' im: P . , i iikr. Klanwlh B oi R< tu^ : . . r v . k v I M •'•- ' -•• Mil - >•> • KlMmth IViim .\ wn 0 1 . . . I SBR g \ ^ m u l Wcllmls En^ :• r I ^ \| V \ • • • I - i I M/ V. u- It; 1 ••••:•• .-.' II-. W Figure 17. Movements of radio- marked sucker W9 on Tule Lake National Wildlife Refuge, California, 1999. 24 Tule Lake- Sucker Radio Telemetry - 1999 Fish: Lost River Sucker " X9" Sex: Female Length 477 mm Tag Location; Anderson Rose Dam Tag Date: 05,1899 Mori. Date, suspected in June 1999 Hn i in Mat h Will •. 1. fackn RadioTclenvtn; i. tfidbU. lkvk « ramLI>. r* Mmw « t K ','. . hmtdth B* m R^ UB* CompK- • n •'• • B % VJI < Kflb . I M i ,• h> tir> l Wetlands Envcntun. I SFft'S \ I , \ ' I K I I \| , ... \| s.\| , \ s Figure 18. Movements of radio- marked sucker X9 on Tule Lake National Wildlife Refuge, California, 1999. 25 June - September - During this period, nearly all suckers ( particularly during July and August) could be found in the DH at the south central portion of Sump 1( A) ( Fig. 4). By connecting the outermost locations of approximately 90% of radio locations, the calculated area of the DH was 188 ha. Suckers using the DH were found in depths ranging from 1.0- 1.3 m ( 39- 50 in) ( Fig. 19). September - December - During this period suckers moved from the DH to the northwest corner of Sump 1( A). As of the writing of this report, ( February 15, 2000) the 13 remaining fish occupy the same area. Recruitment Surveys by Reclamation biologists for larval and juvenile suckers in the Lost River below Anderson- Rose Dam failed to document the presence young of the year fish. Below is a summary of surveys: Date 5/ 25/ 99 6/ 2/ 99 6/ 10/ 99 Result Searches for eggs in gravel below Anderson- Rose Dam revealed eggs in 4 of 5 sites, some of which were viable. Larval surveys conducted at 3 sites ( visual and dip net) from the dam to the wooden bridge were negative. Larval surveys conducted at 5 sites including the dam, 2 and 1 mile downstream, the wooden bridge, and East- West Road were negative. Larval surveys conducted at 2 sites downstream of dam were negative. Water quality pHBln general, pH values were less variable in the DH then areas outside this region ( Fig. 20). In all areas, median pH values remained below 9.5 until early June at which time values outside the DH were frequently above 10.0. pH values were particularly high (> 10.0) in late June through August in ESIB and NWS1A and periodically in the EC and WS1B. pH values in the DH and areas adjacent, remained below 10.0 through September; however, there was a gradual rise in pH values in DH sites from May through September. In late September and early October, DH pH values exceeded all other sites. rem/ reratareBTemperatures in all regions reached a peak in late July through early August with no discernible difference between DH or NDH sites ( Fig. 21). Dissolved oxvgenBDonut Hole sampling station s differed in dissolved oxygen characteristics relative to other areas of the sumps. During the June through August period DH sites ranged from 4.5 to 11.2 mg/ 1 while areas outside this region ranged from 1.1 mg/ 1 to 18.2 mg/ 1 ( Fig. 21). Toward November DH and NDH sites became similar DO dynamics ( Fig. 21). 26 Turbiditvllln general, turbidity values appeared greater in the DH versus areas outside, although some sites particularly in Sump 1( B) were quite variable particularly in June and July. This may have been due to the large amount of filamentous algae in Sump 1( B), potentially interfering with the measurement. Turbidity rose sharply at sites by late October and November ( Fig. 23- 24). 20 >• 1 5 O UJ a UJ DC 10 0 39 41 43 45 47 More DEPTH Figure 19. Water depth used by radio- marked suckers in the " Donut Hole" ( June- August), Tule Lake NWR. California. 27 BJll I U r S o I! Figure 20. pH data collected from " Donut Hole" and non- Donut Hole water quality sampling sites on Tule Lake National Wildlife Refuge, California, 1999. Box and whisker plots represent the median, 25- 75* and 10- 90* percentiles, and outliers. 28 temp rC) S 2 £ ' I j 1 II i 9 E 9 S Figure 21. Water temperatures collected at " Donut Hole" and non- Donut Hole sites on Tule Lake National Wildlife Refuge, California, 1999. Box and whisker plots represent the median, 25- 75^ and 10- 90^ percentiles, and outliers. 29 do ( mgfl) I do ( mg/ l) OP> !• WKamm 01900 gGBM s ' S:' TP" » S i I ! if Figure 22. Dissolved oxygen concentrations at " Donut Hole" and non- Donut Hole sites on Tule Lake National Wildlife Refuge, California, 1999. Box and whisker plots represent the median, 25- 75 and 10- 90* percentiles, and outliers. 30 260.0 -. 240.0 220.0 - 200 0 180.0 => 160.0 H 140.0 - z 120.0 100.0 - 80.0 60.0 40.0 20.0 n n - » NT" —•— Depth ( m) fc= _ 6/ 2 107.00 0.8 Donut Hole Northwest - — .^^^ 6/ 7 77.20 0.8 H •—-^^ ' '—^ 6/ 14 25.30 0.8 6/ 21 24.80 0.8 - 1.0 o o O CJl depth ( m) 260.0 -, 240.0 220 0 200.0 180.0 - 2 160.0 z 140.0 - 120.0 100.0 - 80.0 - 60.0 40.0 20 0 0.0 » NTU — a— Depth ( m) , •=— mmm •= « a 6/ 22 44.00 0.9 Donut Hole West — « — — » - 6/ 28 26.60 08 •— 7/ 6 19.90 08 . ^ m — _ _ _ _ _ _ _ 7/ 13 25.70 0.8 • - _ — r- • 7/ 19 51.40 0.8 1.0 0.5 £ a. T3 0.0 260 0 240.0 - 220.0 - 200.0 - 180.0 i « n n _ H 140.0 - z 120 0 ^ 100.0 • 80 0 60.0 40.0 20.0 - u. u » NTU — m— Depth ( m) 6/ 22 93.70 0.8 6/ 28 95.40 0.7 Donut Hole East 7/ 6 72.70 0.7 7/ 13 32.30 0.7 —•'•"-""* 7/ 19 50.20 0.5 -"— 7/ 28 62.50 0.8 8/ 2 73.30 0.8 \ ^ 8/ 10 18.55 0.8 8/ 19 50.20 0.8 8/ 25 22.20 0.8 8/ 31 58.67 0.7 \ 9/ 8 14.38 0.8 9/ 14 11.03 0.8 9/ 20 7.00 0.7 9/ 29 7.80 0.7 j / A - 10/ 25 51.00 0.7 t - fT u 11/ 23 210.00 0.6 1 0 - 0.5 JZ jepi - 0.0 Figure 23. Turbidity at " Donut Hole" sites on Tule Lake National Wildlife Refuge, California, May to November 1999. 31 260.0 i 240.0 220.0 200.0 180.0 3 160.0 £ 140.0 - 120.0 100.0 80.0 60.0 40.0 20.0 0.0 » NTU —•— Depth ( m) • ^ 6/ 2 81.10 0.8 Donut Hole - — - ^ 6/ 7 49.20 0.8 — • 6/ 14 21.50 0.8 =— 1 6/ 21 24.80 0.8 r 1 0 o p d en depth ( m) 260 0 240.0 • 220.0 - 200.0 . 180.0 - K 160.0 • z 140.0 - 120.0 100.0 80.0 . 60.0 - 40.0 - 20.0 0.0 . t K » TII — a— Depth ( m) B — • 7/ 21 53.30 0.8 .— m-— 7/ 28 40.50 0.8 Donut Hole South _—• 8/ 2 56.80 0 9 » - ^ 8/ 10 17.13 0.9 —• 8/ 18 19.70 0 8 8/ 25 21.73 0.9 ^ \ 8/ 31 64.90 0.8 9/ 8 21.27 0.8 9/ 14 20.80 0.8 9/ 20 29.97 0.8 ^ - • - ^ 9/ 29 49.30 0.8 / / 10/ 25 33.70 0.8 / / 11/ 23 170.00 0.7 1 0 o o d en depth ( m) Figure 23 ( cont.). Turbidity at " Donut Hole" sites on Tule Lake National Wildlife Refuge, California, May- November, 1999. 32 260.0 -, 240.0 - 220.0 200.0 180.0 - 160.0 Z> 140.0 \ z 120.0 - z 100.0 80.0 60.0 40.0 20.0 - 0.0 _ NTU • depth ( m) y 5/ 26 12.30 0.7 6/ 2 58.70 0.8 A- 6/ 7 20.30 0.9 / / 6/ 21 57.40 0.8 // A A\\ 6/ 28 239.0C 0.8 V\ East Sump 1B J s in 81.70 0.7 : / I 7/ 12 10.40 1.0 \| A / \ J I s f 7/ 27 228.00 1.0 \ - V \ 8/ 2 88.00 0.8 8/ 10 40.00 0.9 8/ 18 38.17 0.8 8/ 31 11.30 0.7 9/ 9 7.00 0.7 9/ 14 6.17 0.7 9/ 20 5.83 0.7 • / 10/ 25 44.80 1.0 4-— \ ft . 11/ 23 186.00 0.5 1.0 ? e Q. 0.5 • 0.0 260.0 n 240.0 - 220.0 200.0 180.0 160.0 D 140.0 1— 120 0 z 100^ 0 80.0 60.0 An n 20.0 - 0.0 - —+— NTU —•— depth ( m) —•— 5/ 26 13.70 1.0 _, • —- « - 6/ 2 57.30 1.1 --•— ' \ 6/ 7 41.10 1.1 6/ 21 18.70 1.0 —•— / \ 6/ 28 138.0( 1.0 \ \ / ¥ West Sump 1B - . • — • / 7/ 7 ) 29.90 1.0 A \\ 7/ 12 88.90 1.0 k / \ / 7/ 27 19.00 0.9 / \ / \ 8/ 2 73.00 1.0 L \ \ 8/ 10 5.47 1.0 8/ 18 6.40 1.0 8/ 31 9.20 1.0 9/ 9 8.58 1.0 9/ 14 8.37 0.9 9/ 20 11.73 0.9 / / 10/ 25 39.50 0.7 f 11/ 23 85.00 0.8 1 5 sz Q. - 0 . 5 • - 0.0 260 0 240.0 220.0 - 200.0 - 180.0 160.0 3 140.0 t ; 120.0 100.0 80.0 - 60.0 An n . 20.0 0.0 » NT" — m— Depth ( m) 6/ 2 46.50 0.8 -~ « — 6/ 7 16.10 0.9 —•—. 6/ 14 39.00 0.8 / 6/ 22 9.71 0.8 English Channel Sump 1A 6/ 28 6.79 0.8 \ ^ _ 7/ 13 17.90 0.8 7/ 20 17.60 0.8 7/ 28 26.80 0.8 8/ 10 4.80 0.9 8/ 19 7.33 0.8 8/ 25 6.50 0.8 8/ 31 7.10 0.8 9/ 8 13.34 0.8 ==•== 9/ 20 15.50 0.8 J 9/ 29 22.60 0.7 — y / 10/ 25 98.70 0.8 11/ 23 146.00 0.8 1 5 - 1.0 — 0.5 - g 0.0 260 0 240.0 220 0 - 200.0 - 180.0 - 160.0 => 140.0 - £ 120.0 mnn . 60.0 40.0 - 20.0 u. u J •— NTU —•— Depth ( m) I 6/ 2 36.50 1.2 —•— 6 / 7 12.60 1.2 6/ 14 13.10 1.2 y 6/ 28 7.40 1.1 7/ 6 71.60 1.0 Northwest Sump 1A —•— 7/ 13 5.27 1.1 — » — —•— 7/ 19 28.50 1.1 7/ 28 20.50 1.2 8/ 2 32.10 1.2 ^- B—' 8/ 19 4.50 1.1 / 8/ 25 52.87 1.1 A ' \ 8/ 31 115.67 1.2 ="-•— \ —•*=; 9/ 8 4.10 1.1 1 4- 9/ 14 7.89 1.1 —•— J I \ 9/ 20 12.43 1.1 — « ^ 10/ 25 180.00 1.1 11/ 23 164.00 0.9 1 S d jpth ( m) • 0.5 - o - 0.0 Figure 24. Turbidity at non- Donut Hole sites on Tule Lake National Wildlife Refuge, California, 1999. 33 Discussion Water Quality The area of the DH was delineated from plotted June through September locations of radio-marked suckers ( approximately 188 ha.). The location of the DH could also be seen as an area of relatively turbid water from aerial photographs from August 1998 ( Fig. 25) as well as aerial photographs taken in 1984. It is possible that the combination of 2 factors may cause the observed turbidity in the DH. First, seeps or springs may be present in the area which result in more favorable water quality during summer which attracts suckers as well as other fish species to the area. The resultant concentration offish ( suckers and chubs) may stir the sediments during feeding activities, thereby creating the observed turbidity. The additional turbidity in the DH may inhibit light penetration and the production of algae, thereby reducing photo synthetically elevated pH and the extreme minimum and maximums in DO typical of may water bodies in the Klamath Basin including Tule Lake ( Dileanis et al. 1996). The rise in turbidity at all sites in fall is likely due to the break down of rooted aquatic vegetation which then allows for wind induced wave action to stir the sediments. Other than the DH, all other sites had dense concentrations of rooted aquatic plants and/ or filamentous green algae during summer. June to September DO and pH dynamics in the DH appeared different than at NDH sites ( Figs. 20 and 22). The difference was greatest in early summer with the difference becoming smaller by late summer and essentially disappearing by fall. Whether this water quality difference was a result of the more turbid waters or inflow from springs is unknown. However, attempts by Service hydrologists to model inflows, evapotranspiration, and outflows from the sumps have resulted in a positive imbalance of approximately 21,000 acre- feet of water from April through September. This positive imbalance is greatest in spring and early summer, gradually lessening by summer and essentially disappearing by fall ( Tim Mayer, pers. comm.). If this inflow is occurring, it may explain differences in summer water quality between DH and NDH sites. June to September water quality in the DH may be critical to the over summer survival of suckers in Tule Lake as pH and DO in NDH sites during summer often exceeded the tolerance limits for the fish. DO and pH levels at DH sites were less variable and did not reach the extremes that were reached in NDH sites. The lowest DO measured during June through September at DH sites were 4.83 mg/ 1 ( DHWEST) and 4.96 mg/ 1 ( DHEAST). DO and pH during summer from this study were similar to values collected by Reclamation in 1992 ( Table 3). Buettner and Scoppettone ( 1990) found juvenile suckers only where DO was above 4.5 mg/ 1. It is currently believed that adult suckers become stressed at DO levels below 4.0 mg/ 1 with mortality occurring at or below 2.0 mg/ 1 ( M. Buettner, pers. comm.). The relatively high over- summer survival of radio- marked suckers, compared to suckers radio- marked in Upper Klamath Lake ( M. Buettner, pers. comm), is further evidence of suitable summer water quality conditions in the DH on Tule Lake. 34 Figure 25. " Donut Hole" in Sump 1( A) of Tule Lake NWR. Note visible turbidity of area. 35 Table 3. Mean dissolved oxygen, pH, conductivity, and temperature on Tule Lake National Wildlife Refuge, California, July and August 1992. Data are from 2 sites; 1 site each in Sump 1( A) ( within the ADonut Hole@) and 1( B). All data were from 96 hour continuous readings from Hydrolabs. Data were collected at intervals of 1- 2 hours. ( Data summarized from U. S. Bureau of Reclamation). Site Sump 1( A) Sump ( IB) Depth ( M) < 0.5 0.51- 1.5 > 1.5 < 0.5 0.51- 1.5 > 1.5 pH (± SD) ( 1200- 1700 hrs) 9.32 ± 0.83 n= 81 9.22 ± 0.93 n= 26 8.30 ± 0.71 n= 10 9.65 + 0.44 n= 21 9.79 ± 0.45 n= 7 No data Temp ° C (± SD) ( 1200- 1700 hrs) 21.85 ± 2.84 n= 81 21.53 ± 2.46 n= 26 19.90 ± 1.59 n= 10 22.96+ 1.10 n= 21 22.11 ± 0.51 n= 7 No data Conductivity 500 ± 266 n= 81 598 ± 277 n= 26 859 ± 694 628 ± 148 n= 21 571 ± 74 n= 7 No data DO1 Oof 31 days - - 8 of 21 days - - 1 Proportion of monitored days having a minimum dissolved oxygen level below 5 mg/ 1. ( Data from U. S. Bureau of Reclamation) pH levels in the DH generally remained below 10.0 whereas non DH sites frequently exceeded 10.0 ( Fig. 19). Falter and Cech ( 1991) determined a maximum pH tolerance in shortnose suckers of 9.55+ 0.43 under laboratory conditions, levels generally exceeded in June - September at non DH sites and some DH sites in late summer. Buettner and Scoppettone ( 1990) found juvenile fish in Upper Klamath Lake largely at sites with pH < 9.0, as did Simon et al. ( 1996) in 1994. However, in 1995, Simon et al. ( 1996) found that most juvenile fish ( 54%) were captured in areas of higher pH (> 10.0). Laboratory studies indicate significant mortality of larval and juvenile fish at high pH values (> 9.55) ( Falter and Cech 1991) and 9.92- 10.46 ( Bellerud and Saiki 1995). Previous water quality and fish health studies on the refuge determined that water quality conditions were stressful to aquatic life and was resulting in a high ( up to 37%) proportion offish with deformities ( Dileanis et al. 1996), however, studies of sucker ecology in Tule Lake have indicated that individual fish in the lake have a high condition factor and are free of external parasites ( Scoppettone and Buettner 1995). Bennet ( 1994) recognized this apparent inconsistency, stating, A... the observation that Tule Lake suckers are in better physical condition than Upper Klamath Lake suckers indicates that certain areas of the aquatic system may be of particular importance for the recovery of those species. ® In the case of Tule Lake this Acertain area@ is likely the DH.. Suckers in Tule Lake may be in good condition because of their limited population size, the abundant food resources in this lake, and adequate water quality ( in the DH) to survive the summer period. 36 Sucker movements Although, suckers were relatively sedentary during most periods of the year, they exhibited the ability to make long distance moves in relatively short periods of time, particularly during the April spawning period. The northwest corner of Sump 1( A) receives about 90% of the inflow from the Lost River and spring winds on Tule Lake tend to move large quantities of water through the AEnglish Channels back and forth between Sump 1( A) and 1( B). This movement of water at both locations may explain the movement of fish observed in April and May. Suckers may be attracted to both locations when seeking spawning habitat in spring. Recruitment During the April marking period, most captured suckers appeared to be physiologically ready to spawn; however, only one fish moved into the river. Of 10 radio- marked fish monitored by Reclamation in 1993- 95 no fish attempted to run the Lost River. This low proportion offish that attempt to spawn may have one or several causes or a combination, including: 1. Stress of handling and implanting radio- transmitters so close to the spawning season may prevent fish from becoming reproductively active. 2. Under normal conditions, only a small proportion of Tule Lake suckers may attempt to spawn in any particular year. 3. Flow conditions in or at the mouth of the Lost River may be inadequate to draw the fish into the river. 4. A shallow bar (< 0.3 m) of deposited silt exists between the lake and the mouth of the river which may form a physical barrier to the fish. At the present time, a mandated flow of 30 cfs is released below Anderson- Rose Dam to provide spawning habitat at the Dam. Although this flow is intended to provide suitable spawning conditions at the Dam, these flows may be inadequate to entice fish into the river. It is likely that the historic spring flows in the Lost River were many times higher than current regulated flows. However, given that the fish are largely unsuccessful in spawning and risk additional mortality traversing the river, adult survival may be enhanced by remaining in the lake. Scoppettone and Buettner ( 1995) also observed no radio- marked fish from Clear Lake to move into Willow Creek during the spring spawning period. In this case the authors attributed this result to either capture stress or low stream flows during spring. 37 Habitat use Although the DH is relatively shallow relative to other areas of Tule Lake, use of the DH may be mandatory to ensure over- summer survival. Although deeper waters are available to the fish, especially in the northwest corner of Sump 1( A), DO levels, in particular, likely preclude their use. Suckers did not move out of the DH until October when DO levels began to rise with cooler water temperatures. Although, Sump 1( B) contained suitable water depths and water quality conditions in fall, no suckers were located in this area. It is possible that suckers may prefer not to pass through the pipes connecting the Sumps or the proximity and flow from the Lost River in the northwest corner of Sump 1( A) may make this area more attractive as an over- winter habitat area. The relative lack of water depth in the DH as well as other areas of the sumps is becoming of increasing concern because of the loss of water depth through sedimentation. If suckers require a minimum of 3 ft of water, as is current believed ( M. Buettner, pers. comm.), current rates of sedimentation in the sumps threaten the future suitability of Tule Lake for suckers. Based on a comparison of bathymetric surveys conducted by Reclamation in 1958 and again in 1986, sedimentation has been steadily reducing the water holding capacity of both sumps. Between the 1958 and 1986 surveys ( 28 years), Sump 1( A) has lost 22.4% of its water capacity and Sump 1( B) has lost 30.8% of its capacity due to sedimentation. This would indicate a total mean sedimentation of 11.8 inches over this time period ( U. S. Bureau of Reclamation, unpubl. rep). Over the last several years, an attempt has been made to store additional water in Tule Lake during summer by raising water levels above 4034.60 ft. This increase in water elevations ( between 4034.60 and 4034.90 ft) has somewhat mitigated the loss of depth through sedimentation. However, without reinforcing and raising the levees around the sumps, there is a limit as to how high water elevations can rise. At elevation 4035.50 ft., operating regulations require breaching the sumps into overflow areas ( Sump 2 or 3). Although increased summer operating levels may assist the fish, they may also increase the risk of a flood event requiring the breaching of the sumps with potentially negative impacts to the fish. Acknowledgements The authors are indebted to fisheries biologist from the U. S. Bureau of Reclamation, Klamath Project, especially M. Buettner, B. Peck, and M. Green whom provided and surgically implanted radio transmitters, captured adult suckers, located fish from fixed wing aircraft, and assisted with study design. K. Miller from Klamath Basin National Wildlife Refuge collected telemetry, water quality, and GPS data and ensured all data were collected and coordinated consistent with study design. T. Mayer provide training in the calibration, deployment, and downloading of data from the hydrolabs and assisted with interpretation of water quality data. 38 Personnel Communications Buettner, M., Fisheries Biologist, U. S. Bureau of Reclamation, Klamath Project Office, 6600 Washburn Way, Klamath Falls, Oregon. Mayer, T., Hydrologist, U. S. Fish and Wildlife Service, Portland Regional Office, Lloyd Center, Portland, Oregon. Literature Cited Bellerud, B., and M. K. Saiki. 1995. Tolerance of larval and juvenile Lost River and shortnose suckers to high ph, ammonia concentration, and temperature, and to low dissolved oxygen concentration, National Biological Service, California Pacific Science Center, Dixon 103pp. Bennett, J. K. 1994. Bioassessment of irrigation drain water effects on aquatic resources in the Klamath Basin of California and Oregon. Ph. D Dissertation. University of Washington, Seattle. 197pp. Buettner, M. E., and G. Scoppettone. 1990. Life history and status of catostomids in Upper Klamath Lake, Oregon. National Fisheries Research Center, Reno Field Station, Reno, Nevada, 108pp. Coots, M. 1965. Occurrences of the Lost River sucker, Deltistes luxatus ( Cope), and shortnose sucker, Chasmistes brevirostris ( Cope), in Northern California. Calif. Fish and Game 51: 68- 73. Dileanis, P. D., S. K. Schwarzbach, and J. K. Bennett. 1996. Detailed study of water quality, bottom sediment, and biota associated with irrigation drainage in the Klamath Basin, California and Oregon, 1990- 92. U. S. Geological Survey, Water- Resources Investigations Report 95- 4232, 68pp. Falter, M. A., and J. J. Cech. 1991. Maximum pH tolerance of three Klamath Basin fishes. Copia 4: 1109- 1 111. Simon, D. C, G. R. Hoff, D. J. Logan, and D. F. Markle. 1996. Larval and juvenile ecology of Upper Klamath Lake suckers. Annual Report: 1995, Department of Fisheries and Wildlife, Oregon State Univ., Corvallis. 60pp. 39 Scoppettone, G. G., and M. E. Buettner. 1995. Information on population dynamics and life history of shortnose suckers ( Chasmistes brevirostris) and Lost River suckers ( Deltistes luxatus) in Tule and Clear Lakes. U. S. Geological Survey, Reno Field Station, Reno, Nevada. 79pp. U. S. Bureau of Reclamation. 1998. Lost River and shortnose sucker spawning in Lower Lost River, Oregon, U. S. Bureau of Reclamation, Klamath Falls, Oregon. 1 lpp. . 1993. Lost River { Deltistes luxatus) and shortnose { Chasmistes brevirostris) Sucker Recovery Plan. Portland, Oregon 108pp. Hydrolab Corporation. 1997. DataSondeR 4 and MiniSondeR water quality multiprobes, users manual. Hydrolab Corp., Austin, Texas.

1525. [Image] Summary of ongoing and planned work of the Department of the Interior related to the Klamath River Basin, March 2003


	The Department of the Interior, Klamath River Basin, Work Plans and Reports
	Citation Citation Citation Abstract Copy Title: Summary of ongoing and planned work of the Department of the Interior related to the Klamath River Basin, March 2003 Author: United States. Dept. of the Interior Year: 2003, 2005 The Department of the Interior, Klamath River Basin, Work Plans and Reports Title: Summary of ongoing and planned work of the Department of the Interior related to the Klamath River Basin, March 2003 Author: United States. Dept. of the Interior Year: 2003, 2005 The Department of the Interior, Klamath River Basin, Work Plans and Reports

1526. [Image] IMST review of the USFWS and NMFS 2001 biological opinions on management of the Klamath Reclamation Project and related reports: a report of the Independent Multidisciplinary Science Team, Oregon Plan for Salmon and Watersheds


	This report is a review of scientific research done by various organizations involved in the Klamath Reclamation Project to assess the "status and management of coho salmon in the Klamath River and . . ...
	Citation Citation Citation Abstract Copy Title: IMST review of the USFWS and NMFS 2001 biological opinions on management of the Klamath Reclamation Project and related reports: a report of the Independent Multidisciplinary Science Team, Oregon Plan for Salmon and Watersheds Author: Independent Multidisciplinary Science Team (Oregon) Year: 2003, 2004 This report is a review of scientific research done by various organizations involved in the Klamath Reclamation Project to assess the "status and management of coho salmon in the Klamath River and . . . management of Upper Klamath Lake and its watershed"; "April 16, 2003"; Includes bibliographical references (p. 104-112) Title: IMST review of the USFWS and NMFS 2001 biological opinions on management of the Klamath Reclamation Project and related reports: a report of the Independent Multidisciplinary Science Team, Oregon Plan for Salmon and Watersheds Author: Independent Multidisciplinary Science Team (Oregon) Year: 2003, 2004 This report is a review of scientific research done by various organizations involved in the Klamath Reclamation Project to assess the "status and management of coho salmon in the Klamath River and . . . management of Upper Klamath Lake and its watershed"; "April 16, 2003"; Includes bibliographical references (p. 104-112)

1527. [Image] Klamath River Basin issues and activities


	Klamath River Basin Issues and Activities: An Overview Summary The Klamath River Basin, an area on the California-Oregon border, has become a focal point for local and national discussions on water ...
	Citation Citation Citation Abstract Copy Title: Klamath River Basin issues and activities Author: Kyna Powers Year: 2005, 2008, 2006 Klamath River Basin Issues and Activities: An Overview Summary The Klamath River Basin, an area on the California-Oregon border, has become a focal point for local and national discussions on water management and water scarcity. Water and species management issues were brought to the forefront when severe drought in 2001 exacerbated competition for scarce water resources and generated conflict among several interests - farmers, Indian tribes, commercial and sport fishermen, other recreationists, federal wildlife refuge managers, environmental groups, and state, local, and tribal governments. The conflicts over water distribution and allocation are physically and legally complex, reflecting the varied and sometimes competing uses of limited water supplies in the Basin. For management purposes, the Basin is divided at Iron Gate Dam into the Upper and Lower Basins. As is true in many regions in the West, the federal government plays a prominent role in the Klamath Basin's water management. This role stems from three primary activities: (1) the operation and management of the Bureau of Reclamation's Klamath Water Project and Central Valley Project (e.g., Trinity River dams); (2) management of federal lands in the Basin, including five national wildlife refuges, several national forests, and public lands; and (3) implementation of federal laws, such as the Endangered Species Act (ESA), Clean Water Act (CWA), and National Environmental Policy Act (NEPA). Conflict was sparked in April of 2001 when the Bureau of Reclamation, which has supplied water to farms in the Upper Basin for nearly 100 years, announced that "no water [would] be available" for farms normally receiving water from the Upper Klamath Lake to avoid jeopardizing the existence of three fish species listed as endangered or threatened under the ESA. While some water was subsequently made available to some farmers from other sources (e.g., wells and other Bureau sources), many farmers faced serious hardships. During Reclamation's operations in September of 2002, warm water temperatures and atypically low flows in the lower Klamath contributed to the death of at least 33,000 adult salmonids. This die-off damaged fish stocks and the tribes, commercial fishermen, and recreational anglers that catch Klamath fish. There have been many studies, Biological Opinions, and operating plans over recent years, all of which have been controversial. The events of 2001 and 2002 prompted renewed efforts to resolve water conflicts in the Klamath Basin. Congress has responded to the controversy in a number of ways, including holding oversight hearings and appropriating funds for activities in the area. This report provides an overview of recent conflict in the Klamath Basin, with an emphasis on activities in the Upper Basin, and summarizes some of the activities taking place to improve water supply reliability and fish survival. This report will be updated as events warrant. Title: Klamath River Basin issues and activities Author: Kyna Powers Year: 2005, 2008, 2006 Klamath River Basin Issues and Activities: An Overview Summary The Klamath River Basin, an area on the California-Oregon border, has become a focal point for local and national discussions on water management and water scarcity. Water and species management issues were brought to the forefront when severe drought in 2001 exacerbated competition for scarce water resources and generated conflict among several interests - farmers, Indian tribes, commercial and sport fishermen, other recreationists, federal wildlife refuge managers, environmental groups, and state, local, and tribal governments. The conflicts over water distribution and allocation are physically and legally complex, reflecting the varied and sometimes competing uses of limited water supplies in the Basin. For management purposes, the Basin is divided at Iron Gate Dam into the Upper and Lower Basins. As is true in many regions in the West, the federal government plays a prominent role in the Klamath Basin's water management. This role stems from three primary activities: (1) the operation and management of the Bureau of Reclamation's Klamath Water Project and Central Valley Project (e.g., Trinity River dams); (2) management of federal lands in the Basin, including five national wildlife refuges, several national forests, and public lands; and (3) implementation of federal laws, such as the Endangered Species Act (ESA), Clean Water Act (CWA), and National Environmental Policy Act (NEPA). Conflict was sparked in April of 2001 when the Bureau of Reclamation, which has supplied water to farms in the Upper Basin for nearly 100 years, announced that "no water [would] be available" for farms normally receiving water from the Upper Klamath Lake to avoid jeopardizing the existence of three fish species listed as endangered or threatened under the ESA. While some water was subsequently made available to some farmers from other sources (e.g., wells and other Bureau sources), many farmers faced serious hardships. During Reclamation's operations in September of 2002, warm water temperatures and atypically low flows in the lower Klamath contributed to the death of at least 33,000 adult salmonids. This die-off damaged fish stocks and the tribes, commercial fishermen, and recreational anglers that catch Klamath fish. There have been many studies, Biological Opinions, and operating plans over recent years, all of which have been controversial. The events of 2001 and 2002 prompted renewed efforts to resolve water conflicts in the Klamath Basin. Congress has responded to the controversy in a number of ways, including holding oversight hearings and appropriating funds for activities in the area. This report provides an overview of recent conflict in the Klamath Basin, with an emphasis on activities in the Upper Basin, and summarizes some of the activities taking place to improve water supply reliability and fish survival. This report will be updated as events warrant.

1528. [Image] The Oregon conservation strategy


	v, 419 p.; col.ill.; col.maps; "February 2006"; Foreword by Marla Rae, Chair, Oregon Fish and Wildlife Commission
	Citation Citation Citation Abstract Copy Title: The Oregon conservation strategy Year: 2006 v, 419 p.; col.ill.; col.maps; "February 2006"; Foreword by Marla Rae, Chair, Oregon Fish and Wildlife Commission Title: The Oregon conservation strategy Year: 2006 v, 419 p.; col.ill.; col.maps; "February 2006"; Foreword by Marla Rae, Chair, Oregon Fish and Wildlife Commission

1529. [Image] The Water Report - The ESA, salmon, and Western water law


	Only portions of issues of The Water Report are available in the Klamath Waters Digital Library. See the full report at http://www.thewaterreport.com/.
	Citation Citation Citation Abstract Copy Title: The Water Report - The ESA, salmon, and Western water law Author: Envirotech Publications Year: 2004, 2008, 2006 Only portions of issues of The Water Report are available in the Klamath Waters Digital Library. See the full report at http://www.thewaterreport.com/. Title: The Water Report - The ESA, salmon, and Western water law Author: Envirotech Publications Year: 2004, 2008, 2006 Only portions of issues of The Water Report are available in the Klamath Waters Digital Library. See the full report at http://www.thewaterreport.com/.

1530. [Image] Restoring Harmony in the Klamath Basin


	"January 2003."; Includes bibliographical references (p. 25-28)
	Citation Citation Citation Abstract Copy Title: Restoring Harmony in the Klamath Basin Author: Meiners, Roger E; Kosnik, Lea-Rachel D., 1972- Year: 2003, 2007, 2005 "January 2003."; Includes bibliographical references (p. 25-28) Title: Restoring Harmony in the Klamath Basin Author: Meiners, Roger E; Kosnik, Lea-Rachel D., 1972- Year: 2003, 2007, 2005 "January 2003."; Includes bibliographical references (p. 25-28)

1531. [Image] Ground water hydrology of four proposed project areas in the Klamath Basin, Oregon


	"OF-01-01"
	Citation Citation Citation Abstract Copy Title: Ground water hydrology of four proposed project areas in the Klamath Basin, Oregon Author: Oregon. Water Resources Dept Year: 2001, 2005 "OF-01-01" Title: Ground water hydrology of four proposed project areas in the Klamath Basin, Oregon Author: Oregon. Water Resources Dept Year: 2001, 2005 "OF-01-01"

1532. [Image] Biological assessment of Klamath Project's continuing operations on the endangered Lost River sucker and shortnose sucker


	BIOLOGICAL ASSESSMENT OF KLAMATH PROJECT'S CONTINUING OPERATIONS ON THE ENDANGERED LOST RIVER SUCKER AND SHORTNOSE SUCKER U.S. Bureau of Reclamation Mid-Pacific Region Klamath Basin Area Office Klamath ...
	Citation Citation Citation Abstract Copy Title: Biological assessment of Klamath Project's continuing operations on the endangered Lost River sucker and shortnose sucker Author: United States. Bureau of Reclamation Year: 2001, 2005 BIOLOGICAL ASSESSMENT OF KLAMATH PROJECT'S CONTINUING OPERATIONS ON THE ENDANGERED LOST RIVER SUCKER AND SHORTNOSE SUCKER U.S. Bureau of Reclamation Mid-Pacific Region Klamath Basin Area Office Klamath Falls, Oregon February 13,2001 TABLE OF CONTENTS 1.0 INTRODUCTION 2 2.0 DESCRIPTION OF THE ACTION 3 3.0 DESCRIPTION OF HISTORIC OPERATIONS 6 4.0 ENDANGERED SPECIES POTENTIALLY AFFECTED BY THE KLAMATH PROJECT 16 5.0 ENVIRONMENTAL BASELINE 60 6.0 EFFECTS OF KLAMATH PROJECT ON BALD EAGLES 60 7.0 EFFECTS OF KLAMATH PROJECT ENDANGERED SUCKERS 63 8.0 PROPOSED CRITICAL HABITAT FOR ENDANGERED SUCKERS 82 9.0 CUMULATIVE EFFECTS 84 10.0 DETERMINATION OF EFFECTS 89 11.0 LITERATURE CITED 90 12.0 PERSONAL COMMUNICATIONS 100 13.0 APPENDIX 1 - ESA CONSULTATION REVIEW 101 Title: Biological assessment of Klamath Project's continuing operations on the endangered Lost River sucker and shortnose sucker Author: United States. Bureau of Reclamation Year: 2001, 2005 BIOLOGICAL ASSESSMENT OF KLAMATH PROJECT'S CONTINUING OPERATIONS ON THE ENDANGERED LOST RIVER SUCKER AND SHORTNOSE SUCKER U.S. Bureau of Reclamation Mid-Pacific Region Klamath Basin Area Office Klamath Falls, Oregon February 13,2001 TABLE OF CONTENTS 1.0 INTRODUCTION 2 2.0 DESCRIPTION OF THE ACTION 3 3.0 DESCRIPTION OF HISTORIC OPERATIONS 6 4.0 ENDANGERED SPECIES POTENTIALLY AFFECTED BY THE KLAMATH PROJECT 16 5.0 ENVIRONMENTAL BASELINE 60 6.0 EFFECTS OF KLAMATH PROJECT ON BALD EAGLES 60 7.0 EFFECTS OF KLAMATH PROJECT ENDANGERED SUCKERS 63 8.0 PROPOSED CRITICAL HABITAT FOR ENDANGERED SUCKERS 82 9.0 CUMULATIVE EFFECTS 84 10.0 DETERMINATION OF EFFECTS 89 11.0 LITERATURE CITED 90 12.0 PERSONAL COMMUNICATIONS 100 13.0 APPENDIX 1 - ESA CONSULTATION REVIEW 101

1533. [Image] Making the ESA work better: implementing the 10 point plan - and beyond


	19p.; ill.; Cover title; "June 1997"; "Reprint September 1998"; [Washington, D.C.]: Supt. of Docs., U.S. G.P.O., 1999
	Citation Citation Citation Abstract Copy Title: Making the ESA work better: implementing the 10 point plan - and beyond Year: 1998, 2006, 2005 19p.; ill.; Cover title; "June 1997"; "Reprint September 1998"; [Washington, D.C.]: Supt. of Docs., U.S. G.P.O., 1999 Title: Making the ESA work better: implementing the 10 point plan - and beyond Year: 1998, 2006, 2005 19p.; ill.; Cover title; "June 1997"; "Reprint September 1998"; [Washington, D.C.]: Supt. of Docs., U.S. G.P.O., 1999

1534. [Image] Klamath Project : historic operation


	"November 2000."
	Citation Citation Citation Abstract Copy Title: Klamath Project : historic operation Author: United States. Bureau of Reclamation. Klamath Basin Area Office Year: 2000, 2005 "November 2000." Title: Klamath Project : historic operation Author: United States. Bureau of Reclamation. Klamath Basin Area Office Year: 2000, 2005 "November 2000."

1535. [Image] Nitrogen and phosphorus loading from drained wetlands adjacent to Upper Klamath and Agency Lakes, Oregon


	Two maps digitized separately; Includes bibliographical references (p. 44-49)
	Citation Citation Citation Abstract Copy Title: Nitrogen and phosphorus loading from drained wetlands adjacent to Upper Klamath and Agency Lakes, Oregon Author: Snyder, Daniel T. Year: 1997, 2005, 2004 Two maps digitized separately; Includes bibliographical references (p. 44-49) Title: Nitrogen and phosphorus loading from drained wetlands adjacent to Upper Klamath and Agency Lakes, Oregon Author: Snyder, Daniel T. Year: 1997, 2005, 2004 Two maps digitized separately; Includes bibliographical references (p. 44-49)

1536. [Image] Technical assistance and the Oregon Plan for Salmon and Watersheds: a statewide assessment by the Healthy Streams Partnership


	"November 2002"; 66 p. in various paginations: ill., form -- Executive summary ([6]p.)
	Citation Citation Citation Abstract Copy Title: Technical assistance and the Oregon Plan for Salmon and Watersheds: a statewide assessment by the Healthy Streams Partnership Author: Healthy Streams Partnership Year: 2002, 2007, 2005 "November 2002"; 66 p. in various paginations: ill., form -- Executive summary ([6]p.) Title: Technical assistance and the Oregon Plan for Salmon and Watersheds: a statewide assessment by the Healthy Streams Partnership Author: Healthy Streams Partnership Year: 2002, 2007, 2005 "November 2002"; 66 p. in various paginations: ill., form -- Executive summary ([6]p.)

1537. [Image] Federal Register - Endangered and Threatened Wildlife and Plants; Notice of Revised 90-Day Petition Finding and Initiation of a 5-Year Status Review of the Lost River Sucker and Shortnose Sucker


	We, the U.S. Fish and Wildlife Service (Service), announce a revised 90-day finding for a petition to remove the Lost River sucker [Deltistes luxatus) and shortnose sucker [Chasmistes brevirostris) throughout ...
	Citation Citation Citation Abstract Copy Title: Federal Register - Endangered and Threatened Wildlife and Plants; Notice of Revised 90-Day Petition Finding and Initiation of a 5-Year Status Review of the Lost River Sucker and Shortnose Sucker Author: Larsen, Ron Year: 2004, 2008, 2005 We, the U.S. Fish and Wildlife Service (Service), announce a revised 90-day finding for a petition to remove the Lost River sucker [Deltistes luxatus) and shortnose sucker [Chasmistes brevirostris) throughout their ranges from the Federal List of Threatened and Endangered Wildlife and Plants (List), pursuant to the Endangered Species Act (Act) (16 U.S.C. 1531 et seq.). We find that the petition does not present substantial scientific or commercial information indicating that delisting of the Lost River and shortnose suckers may be warranted. As a result of the 1995, 1996, and 1997 fish die-offs, the endangered suckers experienced significant losses of thousands of adult suckers and have not recovered. Although the petition and information in our files do not provide new information relevant to the status of the Lost River and shortnose suckers, we are initiating a 5-year review of these species under section 4(c)(2)(A) of the Act to consider any new information that has become available as a result of recent actions to reduce threats to the species, and to provide the States, tribes, agencies, university researchers, and the public an opportunity to provide information on the status of the species. We are requesting any new information on the Lost River and shortnose suckers since their original listing as endangered species in 1988 (53 FR 27130) Title: Federal Register - Endangered and Threatened Wildlife and Plants; Notice of Revised 90-Day Petition Finding and Initiation of a 5-Year Status Review of the Lost River Sucker and Shortnose Sucker Author: Larsen, Ron Year: 2004, 2008, 2005 We, the U.S. Fish and Wildlife Service (Service), announce a revised 90-day finding for a petition to remove the Lost River sucker [Deltistes luxatus) and shortnose sucker [Chasmistes brevirostris) throughout their ranges from the Federal List of Threatened and Endangered Wildlife and Plants (List), pursuant to the Endangered Species Act (Act) (16 U.S.C. 1531 et seq.). We find that the petition does not present substantial scientific or commercial information indicating that delisting of the Lost River and shortnose suckers may be warranted. As a result of the 1995, 1996, and 1997 fish die-offs, the endangered suckers experienced significant losses of thousands of adult suckers and have not recovered. Although the petition and information in our files do not provide new information relevant to the status of the Lost River and shortnose suckers, we are initiating a 5-year review of these species under section 4(c)(2)(A) of the Act to consider any new information that has become available as a result of recent actions to reduce threats to the species, and to provide the States, tribes, agencies, university researchers, and the public an opportunity to provide information on the status of the species. We are requesting any new information on the Lost River and shortnose suckers since their original listing as endangered species in 1988 (53 FR 27130)

1538. [Image] Agreement with Indians of Klamath Reservation, Oregon


	"Mr. Moody, of Oregon, from the Committee on Indian Affairs, submitted the following report, to accompany H.R. 8760"
	Citation Citation Citation Abstract Copy Title: Agreement with Indians of Klamath Reservation, Oregon Author: United States. Congress. House. Committee on Indian Affairs Year: 1902, 2004 "Mr. Moody, of Oregon, from the Committee on Indian Affairs, submitted the following report, to accompany H.R. 8760" Title: Agreement with Indians of Klamath Reservation, Oregon Author: United States. Congress. House. Committee on Indian Affairs Year: 1902, 2004 "Mr. Moody, of Oregon, from the Committee on Indian Affairs, submitted the following report, to accompany H.R. 8760"

1539. [Image] Reproductive biology and demographics of endangered Lost River and shortnose suckers in Upper Klamath Lake, Oregon


	We analyzed the reproductive biology and demographics of the Lost River sucker Deltistes luxatus and shortnose sucker Chasmistes brevirostris, two endangered species endemic to the upper Klamath Basin ...
	Citation Citation Citation Abstract Copy Title: Reproductive biology and demographics of endangered Lost River and shortnose suckers in Upper Klamath Lake, Oregon Author: Perkins, David L.; Scoppettone, Gary; Buettner, Mark Year: 2000, 2005 We analyzed the reproductive biology and demographics of the Lost River sucker Deltistes luxatus and shortnose sucker Chasmistes brevirostris, two endangered species endemic to the upper Klamath Basin of Oregon and California, from 1984-1997. Lost River suckers had distinct river and lake shoreline spawning stocks, and individuals of both species commonly spawned in consecutive years. In the Williamson River and lower Sprague River, spawning migration by both species occurred mainly during a 5-week period that started within the first three weeks of April and peaked between mid April and early May, although a separate, earlier (mid March) run of Lost River suckers may also spawn in the upper Sprague River. Migration of both species was several times higher at dawn (0500-0730 h) and evening (1800-2200 h) than other times of the day. Peak migrations almost always corresponded to peaks in water temperature, usually at 10-15°C. Lost River suckers were captured at springs along the east shore of the lake from late February through mid May, with peak spawning usually in mid March to mid April. Shortnose suckers were generally captured at the springs from late March through late May, but the time of peak spawning was not determined. Size and age at maturity was determined by recruitment from a strong year class (1991). Male Lost River suckers began recruitment into the adult population at age 4+ (375-475 mm). Substantial recruitment of females did not begin until age 7+ (510-560 mm). Male and female shortnose suckers began recruitment at age 4+, with the majority offish recruited by age 5+. Males recruited at 270-370 mm; females recruited at 325-425 mm. Fecundity estimates were quite variable ranging from 44,000-236,000 eggs per female Lost River sucker and 18,000-72,000 eggs per female shortnose sucker. In 1984 and 1985, the spawning populations of both species were dominated by large, old individuals, with little indication of recent adult recruitment. In the next 13 years, only one strong year class (1991) recruited into the spawning populations of both species. This year class temporarily boosted population numbers, but annual fish kills from 1995 to 1997 eliminated most adults of both species. Associated with poor water quality caused by the proliferation and decay of blue-green algae Aphanizomenonflos-aquae, these fish kills raise concern that alterations to the lake ecosystem over the past several decades have Perkins et al. Lost River and shortnose suckers 5 increased the magnitude and frequency of poor water quality. As a result, mortality rates of all life stages may have increased, thereby disrupting the species' life history pattern and potentially decreasing long-term population viability. Introduction The Lost River sucker Deltistes luxatus and shortnose sucker Chasmistes brevirostris are large, long-lived suckers endemic to the upper Klamath Basin of Oregon and California. Both species are typically lake dwelling but migrate to tributaries or shoreline springs to spawn (Moyle 1976, Scoppettone and Vinyard 1991). Once extremely abundant (Cope 1884, Gilbert 1898), both species have experienced severe population declines and were federally listed as endangered in 1988 (USFWS 1988). Much of the original habitat of these suckers has been destroyed or altered by conversion of lake areas to agriculture, dams, instream flow diversions, and water quality problems associated with timber harvest, loss of riparian vegetation, livestock grazing, and agricultural practices (USFWS 1988). Knowledge of the life history of Lost River and shortnose suckers is fundamental to recovery of these species. The objective of this report was to present the results of studies conducted from 1987-1998 on the reproductive biology and demographics of Lost River and shortnose suckers, and to compare these results with earlier unpublished data. Study Sites Studies were conducted on Upper Klamath Lake and the lower Williamson-Sprague river system (Figure 1). These waters form the upper portion of the Klamath River Basin in south-central Oregon and represent most remaining native habitat of Lost River and shortnose suckers. Upper Klamath Lake is a remnant of pluvial Lake Modoc that included eight major basins and encompassed 2,839 km2 (Dicken 1980). Today, Upper Klamath Lake serves as a storage reservoir that provides water for agricultural irrigation, waterfowl refuges, instream flow requirements of anadromous fish, and hydroelectric power generation. At full capacity, the lake covers approximately 360 km2 and has an average depth of 2.4 m. Most deeper water (3-12 m) is restricted to narrow trenches along the western shore. Lake elevation is controlled at the outlet by Link River Title: Reproductive biology and demographics of endangered Lost River and shortnose suckers in Upper Klamath Lake, Oregon Author: Perkins, David L.; Scoppettone, Gary; Buettner, Mark Year: 2000, 2005 We analyzed the reproductive biology and demographics of the Lost River sucker Deltistes luxatus and shortnose sucker Chasmistes brevirostris, two endangered species endemic to the upper Klamath Basin of Oregon and California, from 1984-1997. Lost River suckers had distinct river and lake shoreline spawning stocks, and individuals of both species commonly spawned in consecutive years. In the Williamson River and lower Sprague River, spawning migration by both species occurred mainly during a 5-week period that started within the first three weeks of April and peaked between mid April and early May, although a separate, earlier (mid March) run of Lost River suckers may also spawn in the upper Sprague River. Migration of both species was several times higher at dawn (0500-0730 h) and evening (1800-2200 h) than other times of the day. Peak migrations almost always corresponded to peaks in water temperature, usually at 10-15°C. Lost River suckers were captured at springs along the east shore of the lake from late February through mid May, with peak spawning usually in mid March to mid April. Shortnose suckers were generally captured at the springs from late March through late May, but the time of peak spawning was not determined. Size and age at maturity was determined by recruitment from a strong year class (1991). Male Lost River suckers began recruitment into the adult population at age 4+ (375-475 mm). Substantial recruitment of females did not begin until age 7+ (510-560 mm). Male and female shortnose suckers began recruitment at age 4+, with the majority offish recruited by age 5+. Males recruited at 270-370 mm; females recruited at 325-425 mm. Fecundity estimates were quite variable ranging from 44,000-236,000 eggs per female Lost River sucker and 18,000-72,000 eggs per female shortnose sucker. In 1984 and 1985, the spawning populations of both species were dominated by large, old individuals, with little indication of recent adult recruitment. In the next 13 years, only one strong year class (1991) recruited into the spawning populations of both species. This year class temporarily boosted population numbers, but annual fish kills from 1995 to 1997 eliminated most adults of both species. Associated with poor water quality caused by the proliferation and decay of blue-green algae Aphanizomenonflos-aquae, these fish kills raise concern that alterations to the lake ecosystem over the past several decades have Perkins et al. Lost River and shortnose suckers 5 increased the magnitude and frequency of poor water quality. As a result, mortality rates of all life stages may have increased, thereby disrupting the species' life history pattern and potentially decreasing long-term population viability. Introduction The Lost River sucker Deltistes luxatus and shortnose sucker Chasmistes brevirostris are large, long-lived suckers endemic to the upper Klamath Basin of Oregon and California. Both species are typically lake dwelling but migrate to tributaries or shoreline springs to spawn (Moyle 1976, Scoppettone and Vinyard 1991). Once extremely abundant (Cope 1884, Gilbert 1898), both species have experienced severe population declines and were federally listed as endangered in 1988 (USFWS 1988). Much of the original habitat of these suckers has been destroyed or altered by conversion of lake areas to agriculture, dams, instream flow diversions, and water quality problems associated with timber harvest, loss of riparian vegetation, livestock grazing, and agricultural practices (USFWS 1988). Knowledge of the life history of Lost River and shortnose suckers is fundamental to recovery of these species. The objective of this report was to present the results of studies conducted from 1987-1998 on the reproductive biology and demographics of Lost River and shortnose suckers, and to compare these results with earlier unpublished data. Study Sites Studies were conducted on Upper Klamath Lake and the lower Williamson-Sprague river system (Figure 1). These waters form the upper portion of the Klamath River Basin in south-central Oregon and represent most remaining native habitat of Lost River and shortnose suckers. Upper Klamath Lake is a remnant of pluvial Lake Modoc that included eight major basins and encompassed 2,839 km2 (Dicken 1980). Today, Upper Klamath Lake serves as a storage reservoir that provides water for agricultural irrigation, waterfowl refuges, instream flow requirements of anadromous fish, and hydroelectric power generation. At full capacity, the lake covers approximately 360 km2 and has an average depth of 2.4 m. Most deeper water (3-12 m) is restricted to narrow trenches along the western shore. Lake elevation is controlled at the outlet by Link River

1540. [Image] Farming practices and water quality in the Upper Klamath Basin : final report to the California State Water Resources Control Board : 205j program


	Summary The Upper Klamath Basin (UKB) is a high desert region straddling the California-Oregon border east of the Cascade Range. Irrigation and other agricultural practices in the U. S. Bureau of Reclamation's ...
	Citation Citation Citation Abstract Copy Title: Farming practices and water quality in the Upper Klamath Basin : final report to the California State Water Resources Control Board : 205j program Author: Danosky, Earl; Kaffka, Stephen Year: 2002, 2007, 2006 Summary The Upper Klamath Basin (UKB) is a high desert region straddling the California-Oregon border east of the Cascade Range. Irrigation and other agricultural practices in the U. S. Bureau of Reclamation's Klamath Project may result in impaired surface water quality, reducing its use for wildlife and fish in important national wildlife refuges that receive drainage water from farms, and in the Klamath River. By 2004, a system of total maximum daily loads (TMDL) for nutrients must be established for the Klamath River. To investigate the relationships among agricultural practices and surface water quality in the Upper Klamath Basin, a two year reconnaissance survey of surface water and agricultural tile drain locations, focusing on nitrogen and phosphorus concentrations and mass transfers was conducted. Data was collected at 18 surface locations and 10 tile drain locations. Triplicate samples were taken every ten days during the growing season (April through October) and one or two times a month during the remainder of the months, depending on opportunity. No samples were taken from tile drains during the winter months because there was no irrigation and drainage during that period. Water samples were analyzed for phosphorus (total P, soluble reactive P, total filterable P, and particulate P) and nitrogen (total N, soluble N, Soluble organic N, total filterable N, particulate N, and ammonia N), temperature, pH and electrical conductivity, a measure of salinity or total dissolved solids. Analyses of data, including data quality, estimates of the transfer of nutrients in surface waters in the region, and hypotheses about the relationship between agriculture and water quality are reported. 1. The salt and nutrient content of surface waters increases nearly threefold as water moves through the watershed from the Lost River and J canal diversion to the Klamath Straits Drain. Mean ECW levels in input waters at the J canal diversion were approximately 250 \iS cm1, while water sampled at the D pump increased to 600 ^S cm"1 on average over the sample period. By the time water reenters the Klamath River, salt concentrations have increased to approximately 700 jaS cm1. 2. The ECW values observed in subsurface tile drains were higher on average than in input waters and surface waters elsewhere in the region, especially in the Lease Lands area of the Tulelake Irrigation District (TID). ECW values averaged approximately 2,500 ^S cm"1 . Recycling irrigation water through soils in the TID increases the salinity of the water, especially by the time it reaches and is reused in the Lease Lands area of the Tulelake National Wildlife Refuge (TLNWR). Soils in this part of the Klamath Project area are naturally high in salt. 3. Water temperatures in agricultural subsurface tile drains were significantly lower than surface water temperatures during the growing season when tile drains were active. pH values in tile drains were lower than surface water values. The temperature and pH of tile drains does not influence surface water values. 1. 4. For total phosphorus (TP) input waters at the J canal irrigation diversion for the TED averaged approximately 0.27 mg L1 for the two years reported. Water leaving the Tulelake Sumps at the D pump increases to 0.33 mg L1. Water leaving the Lower Klamath National Wildlife Refuge (LKNWR) sampled at the start of the Klamath Straits Drain, averaged 0.33 mg L1, similar to those at the D pump. TP increased further to 0.40 mg L"1 a the end of the Klamath Straits Drain. The overall increase in P concentration in surface waters was much less than for salt, suggesting that processes other than simple enrichment are occurring, particularly those associated with the exchange of sedimentary P and aquatic plant species. TN increases from 2.3 mg L"1 to 4.0 mg L1 over the same pathway. Atomic ratios (TN:TP) of surface water samples remain constant at approximately 10:1 throughout the system, suggesting that the amount of sediment and other small particulate matter in surface waters affects the values observed. The amount of sediment is influenced in part by the agitation of surface water as it passes through pumps and over weirs. 5. The average seasonal TP value in tile drains beneath farm fields is approximately 0.34 mg L"1 . While average total P values in subsurface tile drains were not different from those found at the D pump and the LKNWR outlet, the range in values was great (0.1 to 0.8 mg L1). Similarly, high NO3 -N values were observed at times in tile drains. Very high values in tile drains lead to the inference that some fertilizer N and P is lost in drainage water, combined with nutrients derived from decaying soil organic matter. The amount estimated as lost is much less than the amount of surplus fertilizer P applied and the amount of P surmised to be mineralized from decaying soil organic matter. P from fertilizer and decaying organic matter appears to be accumulating in soils and lake sediments in the region. 6. Ammonia N concentrations are at or below the limit of detection in subsurface agricultural tile lines and one to two orders of magnitude below the values observed in surface soils. Un ionized ammonia increases with temperature. Values above 0.25 mg L1 were observed in late summer at several locations. 7. Some leaching of soluble salts and nutrients is unavoidable when crops are irrigated. P fertilizer is applied at rates higher than crop removal, while fertilizer n is applied at rates less than crop removal. Reduced fertilizer use can help bring P inputs and outputs into balance and may reduce further any avoidable losses of P. This objective should be the subject of an agronomic research program in the region. 8. Surface waters entering the TDD, the TLNWR, and the LKNWR are already enriched with N and P. It seems unlikely that reducing N and P losses from farming in the TID, if possible, would influence surface water quality sufficiently to make them significantly less eutrophic. For P, the hypothesized threshold concentration limiting algae growth in fresh waters is 5 to 25 times smaller than the values observed in waters entering the TID for irrigation use. The addition of 1. nutrients from agriculture probably does not influence significantly surface water quality in the region. Wetland sediments, large amounts of organic matter in soils, and water introduced for irrigation contain essentially unlimited amounts of nutrients for aquatic plant growth. It is not clear how this circumstance could be changed under any reasonable time frame, if ever. 9. Using a TMDL approach may not result in reduced amounts of nutrients returned to the Klamath River because wetlands and farming practices in the southern portion of the Klamath Project result in the net removal of nutrients from the waters diverted for irrigation on a yearly basis, compared to allowing the same amount of water simply to flow down the river unused. Because of large errors of estimation for the amounts of water transferred, combined with smaller errors associated with estimating nutrient concentrations in water samples, and with year to year climate variation, TMDLs may not be an effective or efficient means of reducing nutrients in return flows to the Klamath River. Rational confidence limits for TMDLs may have to be too broad to be effective. Recycling of some drainage water for irrigation would reduce the amount of nutrients returned to the river more effectively than implementing a TMDL program. Title: Farming practices and water quality in the Upper Klamath Basin : final report to the California State Water Resources Control Board : 205j program Author: Danosky, Earl; Kaffka, Stephen Year: 2002, 2007, 2006 Summary The Upper Klamath Basin (UKB) is a high desert region straddling the California-Oregon border east of the Cascade Range. Irrigation and other agricultural practices in the U. S. Bureau of Reclamation's Klamath Project may result in impaired surface water quality, reducing its use for wildlife and fish in important national wildlife refuges that receive drainage water from farms, and in the Klamath River. By 2004, a system of total maximum daily loads (TMDL) for nutrients must be established for the Klamath River. To investigate the relationships among agricultural practices and surface water quality in the Upper Klamath Basin, a two year reconnaissance survey of surface water and agricultural tile drain locations, focusing on nitrogen and phosphorus concentrations and mass transfers was conducted. Data was collected at 18 surface locations and 10 tile drain locations. Triplicate samples were taken every ten days during the growing season (April through October) and one or two times a month during the remainder of the months, depending on opportunity. No samples were taken from tile drains during the winter months because there was no irrigation and drainage during that period. Water samples were analyzed for phosphorus (total P, soluble reactive P, total filterable P, and particulate P) and nitrogen (total N, soluble N, Soluble organic N, total filterable N, particulate N, and ammonia N), temperature, pH and electrical conductivity, a measure of salinity or total dissolved solids. Analyses of data, including data quality, estimates of the transfer of nutrients in surface waters in the region, and hypotheses about the relationship between agriculture and water quality are reported. 1. The salt and nutrient content of surface waters increases nearly threefold as water moves through the watershed from the Lost River and J canal diversion to the Klamath Straits Drain. Mean ECW levels in input waters at the J canal diversion were approximately 250 \iS cm1, while water sampled at the D pump increased to 600 ^S cm"1 on average over the sample period. By the time water reenters the Klamath River, salt concentrations have increased to approximately 700 jaS cm1. 2. The ECW values observed in subsurface tile drains were higher on average than in input waters and surface waters elsewhere in the region, especially in the Lease Lands area of the Tulelake Irrigation District (TID). ECW values averaged approximately 2,500 ^S cm"1 . Recycling irrigation water through soils in the TID increases the salinity of the water, especially by the time it reaches and is reused in the Lease Lands area of the Tulelake National Wildlife Refuge (TLNWR). Soils in this part of the Klamath Project area are naturally high in salt. 3. Water temperatures in agricultural subsurface tile drains were significantly lower than surface water temperatures during the growing season when tile drains were active. pH values in tile drains were lower than surface water values. The temperature and pH of tile drains does not influence surface water values. 1. 4. For total phosphorus (TP) input waters at the J canal irrigation diversion for the TED averaged approximately 0.27 mg L1 for the two years reported. Water leaving the Tulelake Sumps at the D pump increases to 0.33 mg L1. Water leaving the Lower Klamath National Wildlife Refuge (LKNWR) sampled at the start of the Klamath Straits Drain, averaged 0.33 mg L1, similar to those at the D pump. TP increased further to 0.40 mg L"1 a the end of the Klamath Straits Drain. The overall increase in P concentration in surface waters was much less than for salt, suggesting that processes other than simple enrichment are occurring, particularly those associated with the exchange of sedimentary P and aquatic plant species. TN increases from 2.3 mg L"1 to 4.0 mg L1 over the same pathway. Atomic ratios (TN:TP) of surface water samples remain constant at approximately 10:1 throughout the system, suggesting that the amount of sediment and other small particulate matter in surface waters affects the values observed. The amount of sediment is influenced in part by the agitation of surface water as it passes through pumps and over weirs. 5. The average seasonal TP value in tile drains beneath farm fields is approximately 0.34 mg L"1 . While average total P values in subsurface tile drains were not different from those found at the D pump and the LKNWR outlet, the range in values was great (0.1 to 0.8 mg L1). Similarly, high NO3 -N values were observed at times in tile drains. Very high values in tile drains lead to the inference that some fertilizer N and P is lost in drainage water, combined with nutrients derived from decaying soil organic matter. The amount estimated as lost is much less than the amount of surplus fertilizer P applied and the amount of P surmised to be mineralized from decaying soil organic matter. P from fertilizer and decaying organic matter appears to be accumulating in soils and lake sediments in the region. 6. Ammonia N concentrations are at or below the limit of detection in subsurface agricultural tile lines and one to two orders of magnitude below the values observed in surface soils. Un ionized ammonia increases with temperature. Values above 0.25 mg L1 were observed in late summer at several locations. 7. Some leaching of soluble salts and nutrients is unavoidable when crops are irrigated. P fertilizer is applied at rates higher than crop removal, while fertilizer n is applied at rates less than crop removal. Reduced fertilizer use can help bring P inputs and outputs into balance and may reduce further any avoidable losses of P. This objective should be the subject of an agronomic research program in the region. 8. Surface waters entering the TDD, the TLNWR, and the LKNWR are already enriched with N and P. It seems unlikely that reducing N and P losses from farming in the TID, if possible, would influence surface water quality sufficiently to make them significantly less eutrophic. For P, the hypothesized threshold concentration limiting algae growth in fresh waters is 5 to 25 times smaller than the values observed in waters entering the TID for irrigation use. The addition of 1. nutrients from agriculture probably does not influence significantly surface water quality in the region. Wetland sediments, large amounts of organic matter in soils, and water introduced for irrigation contain essentially unlimited amounts of nutrients for aquatic plant growth. It is not clear how this circumstance could be changed under any reasonable time frame, if ever. 9. Using a TMDL approach may not result in reduced amounts of nutrients returned to the Klamath River because wetlands and farming practices in the southern portion of the Klamath Project result in the net removal of nutrients from the waters diverted for irrigation on a yearly basis, compared to allowing the same amount of water simply to flow down the river unused. Because of large errors of estimation for the amounts of water transferred, combined with smaller errors associated with estimating nutrient concentrations in water samples, and with year to year climate variation, TMDLs may not be an effective or efficient means of reducing nutrients in return flows to the Klamath River. Rational confidence limits for TMDLs may have to be too broad to be effective. Recycling of some drainage water for irrigation would reduce the amount of nutrients returned to the river more effectively than implementing a TMDL program.

1541. [Image] Crater Lake market assessment


	ill., maps; "Final report"--Cover; "January 1992."
	Citation Citation Citation Abstract Copy Title: Crater Lake market assessment Author: University of Oregon; Department of Planning, Public Policy, and Management; Community Planning Workshop Year: 1922, 2010 ill., maps; "Final report"--Cover; "January 1992." Title: Crater Lake market assessment Author: University of Oregon; Department of Planning, Public Policy, and Management; Community Planning Workshop Year: 1922, 2010 ill., maps; "Final report"--Cover; "January 1992."

1542. [Image] The Chemical and biological impact of Klamath Marsh on the Williamson River, Oregon


	A comparative study of the Williamson River (before and after passage through Klamath Marsh) and the Sprague River (which is a major tributary of the Williamson River) in South Central Oregon has provided ...
	Citation Citation Citation Abstract Copy Title: The Chemical and biological impact of Klamath Marsh on the Williamson River, Oregon Author: Perdue, Edward M. Year: 1981, 2005 A comparative study of the Williamson River (before and after passage through Klamath Marsh) and the Sprague River (which is a major tributary of the Williamson River) in South Central Oregon has provided substantial insight into the effects of a marsh environment on the transport of iron and aquatic humus in river water. In the Sprague River and in the pre-marsh Williamson River, iron is transported primarily as 0.80 ym suspended particulate material. In Klamath Marsh, this coarse particulate material is "weathered11, yielding iron-aquatic humus "complexes'1. Thus, most iron and aquatic humus in the post-marsh Williamson River are in the 0.025 ?m size fraction. Presumably, other trace metals would be similarly affected. Klamath Marsh serves as an important source of biologically derived solutes such as amino acids and sugars. Fractionation studies have shown that amino acids are almost exclusively humic-bound in the Will-iamson River system, while sugars may be present as either polysacchar-ides (PS) or humic-bound saccharides (HS). The PS/HS ratio may reflect the relative importance of autochthonous and allochthonous sources of sugars. Major solute composition strongly indicates that ground waters flowing into the pre-marsh Williamson River and the Sprague River are derived from a different source than are ground waters which enter the post-marsh Williamson River from Big Springs, Spring Creek, and from unidentified springs below Klamath Marsh. Nutrient concentrations (H4SiO4, NO3, PO43) are significantly higher in spring waters than elsewhere in the system. While nitrate levels (3-11 ?m) were somewhat low, phosphate levels (1-3 ?m) were quite high throughout the Williamson River system. There was some evidence for nitrogen limitation of algal growth in the pre-marsh Williamson River. While Fragilaria construens was dominant throughout the Williamson River system, several Navicula spp. were restricted to the pre-marsh Williamson River and several Fragilaria spp. and Nitzschia, spp. were found only in the post-marsh Williamson River. In Upper Klamath Lake, Stephanodiscus astrea minuta, Fragilaria construens, and Aphanizomenon flos-aquae appeared in succession, with nuisance blooms of the latter organism occurring July-November. The cessation of flow of humic-rich water from Klamath Marsh during the summer months drastically decreased the flux of aquatic humus, iron, amino acids, and other marsh-derived solutes in the post-marsh Williamson River. At the time of cessation of flow from Klamath Marsh, nuisance blooms of Aphanizomenon flos-aquae appeared in Upper Klamath Lake. Furthermore, when flow from the marsh was re-established with the first major winter rains in November or December, Aphanizomenon flos-aquae abruptly ceased to grow in Upper Klamath Lake. Further studies are planned to determine whether this correlation is causal or coincidental. Title: The Chemical and biological impact of Klamath Marsh on the Williamson River, Oregon Author: Perdue, Edward M. Year: 1981, 2005 A comparative study of the Williamson River (before and after passage through Klamath Marsh) and the Sprague River (which is a major tributary of the Williamson River) in South Central Oregon has provided substantial insight into the effects of a marsh environment on the transport of iron and aquatic humus in river water. In the Sprague River and in the pre-marsh Williamson River, iron is transported primarily as 0.80 ym suspended particulate material. In Klamath Marsh, this coarse particulate material is "weathered11, yielding iron-aquatic humus "complexes'1. Thus, most iron and aquatic humus in the post-marsh Williamson River are in the 0.025 ?m size fraction. Presumably, other trace metals would be similarly affected. Klamath Marsh serves as an important source of biologically derived solutes such as amino acids and sugars. Fractionation studies have shown that amino acids are almost exclusively humic-bound in the Will-iamson River system, while sugars may be present as either polysacchar-ides (PS) or humic-bound saccharides (HS). The PS/HS ratio may reflect the relative importance of autochthonous and allochthonous sources of sugars. Major solute composition strongly indicates that ground waters flowing into the pre-marsh Williamson River and the Sprague River are derived from a different source than are ground waters which enter the post-marsh Williamson River from Big Springs, Spring Creek, and from unidentified springs below Klamath Marsh. Nutrient concentrations (H4SiO4, NO3, PO43) are significantly higher in spring waters than elsewhere in the system. While nitrate levels (3-11 ?m) were somewhat low, phosphate levels (1-3 ?m) were quite high throughout the Williamson River system. There was some evidence for nitrogen limitation of algal growth in the pre-marsh Williamson River. While Fragilaria construens was dominant throughout the Williamson River system, several Navicula spp. were restricted to the pre-marsh Williamson River and several Fragilaria spp. and Nitzschia, spp. were found only in the post-marsh Williamson River. In Upper Klamath Lake, Stephanodiscus astrea minuta, Fragilaria construens, and Aphanizomenon flos-aquae appeared in succession, with nuisance blooms of the latter organism occurring July-November. The cessation of flow of humic-rich water from Klamath Marsh during the summer months drastically decreased the flux of aquatic humus, iron, amino acids, and other marsh-derived solutes in the post-marsh Williamson River. At the time of cessation of flow from Klamath Marsh, nuisance blooms of Aphanizomenon flos-aquae appeared in Upper Klamath Lake. Furthermore, when flow from the marsh was re-established with the first major winter rains in November or December, Aphanizomenon flos-aquae abruptly ceased to grow in Upper Klamath Lake. Further studies are planned to determine whether this correlation is causal or coincidental.

1543. [Image] Soils of the Klamath Indian Reservation; interim report, June 11, 1958


	TABLE OF CONTENTS PART I INTRODUCTION 18 - 11 History and ethnology 18 Irrigated area table 19 Cultural geography 19 General physiographic features 262e . .3 Physiographic areas and farming 1d CLIMATE ...
	Citation Citation Citation Abstract Copy Title: Soils of the Klamath Indian Reservation; interim report, June 11, 1958 Author: United States. Bureau of Indian Affairs Year: 1958, 2005, 2004 TABLE OF CONTENTS PART I INTRODUCTION 18 - 11 History and ethnology 18 Irrigated area table 19 Cultural geography 19 General physiographic features 262e . .3 Physiographic areas and farming 1d CLIMATE 182 - 18 Climatic table, Sprague River, Oregon 185 Precipitation table , Chiloquin, Oregon 186 Temperature table, Chiloquin, Oregon 187 Climatic table, Fort Klamath, Oregon 188 VEGETATION 189 - 25 GEOLOGY 196 - 51 Hydrography: rivers, lakes, marshes, ground water 196 Relief and geological formations. 262e .32 Diatomite - tuff formation 262e . 1c4 Pliocene sediments of the Modoc Point area 262e.. 37 Faulted tuff formation 1c9 Pumice tuff formation.. 1d0 Pumice mantle and pumice flows ........ 262e.... .........40 Table of chemical analyses of pumice and scoria 1d5 Geology Map 262e . 262e 221 BIBLIOGRAPHY 262e 262e...52 PART II DESCRIPTIONS OF SOILS 223 - 60 Classification and survey 262e 262e.. 262e... 53 Soil profile and nomenclature. .... 262e...53 Chestnut Soils 262e 224 "Western" Brown Forest Soils 225 Regosol Soils . . 262e. 262e......56 Solonetz Soils 262e.....57 Halomorphic Soils 262e 228 Hydromorphic Soils 262e... 229 Soil Association Map 262e 229 KEY TO SOIL SERIES 262e61 - 63 SOIL SERIES AND MAPPING UNIT DESCRIPTIONS 134 ~ 254 APPENDIX 1955 - 297 Soil Series and mapping unit index. 2620. . . . 255 Glossary of terms 263f 262e. . . . 272 Table of soil analyses (Oregon State College)... 1989 Table of irrigation water quality (Oregon State College) 1990 Table of conductivity and reaction. . . . 1991 Table of resistance of saturated paste 262e296 Title: Soils of the Klamath Indian Reservation; interim report, June 11, 1958 Author: United States. Bureau of Indian Affairs Year: 1958, 2005, 2004 TABLE OF CONTENTS PART I INTRODUCTION 18 - 11 History and ethnology 18 Irrigated area table 19 Cultural geography 19 General physiographic features 262e . .3 Physiographic areas and farming 1d CLIMATE 182 - 18 Climatic table, Sprague River, Oregon 185 Precipitation table , Chiloquin, Oregon 186 Temperature table, Chiloquin, Oregon 187 Climatic table, Fort Klamath, Oregon 188 VEGETATION 189 - 25 GEOLOGY 196 - 51 Hydrography: rivers, lakes, marshes, ground water 196 Relief and geological formations. 262e .32 Diatomite - tuff formation 262e . 1c4 Pliocene sediments of the Modoc Point area 262e.. 37 Faulted tuff formation 1c9 Pumice tuff formation.. 1d0 Pumice mantle and pumice flows ........ 262e.... .........40 Table of chemical analyses of pumice and scoria 1d5 Geology Map 262e . 262e 221 BIBLIOGRAPHY 262e 262e...52 PART II DESCRIPTIONS OF SOILS 223 - 60 Classification and survey 262e 262e.. 262e... 53 Soil profile and nomenclature. .... 262e...53 Chestnut Soils 262e 224 "Western" Brown Forest Soils 225 Regosol Soils . . 262e. 262e......56 Solonetz Soils 262e.....57 Halomorphic Soils 262e 228 Hydromorphic Soils 262e... 229 Soil Association Map 262e 229 KEY TO SOIL SERIES 262e61 - 63 SOIL SERIES AND MAPPING UNIT DESCRIPTIONS 134 ~ 254 APPENDIX 1955 - 297 Soil Series and mapping unit index. 2620. . . . 255 Glossary of terms 263f 262e. . . . 272 Table of soil analyses (Oregon State College)... 1989 Table of irrigation water quality (Oregon State College) 1990 Table of conductivity and reaction. . . . 1991 Table of resistance of saturated paste 262e296

1544. [Image] Water-quality data from 2002 to 2003 and analysis of data gaps for development of total maximum daily loads in the Lower Klamath River basin, California


	By Lorraine E. Flint, Alan L. Flint, Debra S. Curry, Stewart A. Rounds, and Micelis C. Doyle Abstract The U.S. Geological Survey (USGS) collected water? quality data during 2002 and 2003 In ...
	Citation Citation Citation Abstract Copy Title: Water-quality data from 2002 to 2003 and analysis of data gaps for development of total maximum daily loads in the Lower Klamath River basin, California Author: Flint, Lorraine E.; Flint, Alan L.; Curry, Debra S.; Rounds, Stewart A.; Doyle, Micelis C. Year: 2004, 2006, 2005 By Lorraine E. Flint, Alan L. Flint, Debra S. Curry, Stewart A. Rounds, and Micelis C. Doyle Abstract The U.S. Geological Survey (USGS) collected water? quality data during 2002 and 2003 In the Lower Klamath River Basin, in northern California, to support studies of river conditions as they pertain to the viability of Chinook and Coho salmon and endangered suckers. To address the data needs of the North Coast Regional Water Quality Control Board for the development of Total Maximum Daily Loads (TMDLs), water temperature, dissolved oxygen, specific conductance, and pH were continuously monitored at sites on the Klamath, Trinity, Shasta, and Lost Rivers. Water-quality samples were collected and analyzed for selected nutrients, organic carbon, chlorophyll-a, pheophytin-a, and trace elements. Sediment oxygen demand was measured on the Shasta River. Results of analysis of the data collected were used to identify locations in the Lower Klamath River Basin and periods of time during 200 Title: Water-quality data from 2002 to 2003 and analysis of data gaps for development of total maximum daily loads in the Lower Klamath River basin, California Author: Flint, Lorraine E.; Flint, Alan L.; Curry, Debra S.; Rounds, Stewart A.; Doyle, Micelis C. Year: 2004, 2006, 2005 By Lorraine E. Flint, Alan L. Flint, Debra S. Curry, Stewart A. Rounds, and Micelis C. Doyle Abstract The U.S. Geological Survey (USGS) collected water? quality data during 2002 and 2003 In the Lower Klamath River Basin, in northern California, to support studies of river conditions as they pertain to the viability of Chinook and Coho salmon and endangered suckers. To address the data needs of the North Coast Regional Water Quality Control Board for the development of Total Maximum Daily Loads (TMDLs), water temperature, dissolved oxygen, specific conductance, and pH were continuously monitored at sites on the Klamath, Trinity, Shasta, and Lost Rivers. Water-quality samples were collected and analyzed for selected nutrients, organic carbon, chlorophyll-a, pheophytin-a, and trace elements. Sediment oxygen demand was measured on the Shasta River. Results of analysis of the data collected were used to identify locations in the Lower Klamath River Basin and periods of time during 200

1545. [Image] Western water supply : hearing before the Committee on Energy and Natural Resources, United States Senate, One Hundred Eighth Congress, second session, to receive testimony regarding water supply issues in the arid West, March 9, 2004


	CONTENTS STATEMENTS Page American Farm Bureau Federation 26963 Bell, Craig, Executive Director, Western States Water Council 26945 Domenici, Hon. Pete V., U.S. Senator From New Mexico 2691 Gaibler, Floyd, ...
	Citation Citation Citation Abstract Copy Title: Western water supply : hearing before the Committee on Energy and Natural Resources, United States Senate, One Hundred Eighth Congress, second session, to receive testimony regarding water supply issues in the arid West, March 9, 2004 Author: United States. Congress. Senate. Committee on Energy and Natural Resources Year: 2004, 2005 CONTENTS STATEMENTS Page American Farm Bureau Federation 26963 Bell, Craig, Executive Director, Western States Water Council 26945 Domenici, Hon. Pete V., U.S. Senator From New Mexico 2691 Gaibler, Floyd, Deputy Undersecretary for Farm and Foreign Agricultural Services, Department of Agriculture 26932 Grisoli, Brigadier General William T., Commander, Northwestern Division, U.S. Army Corps of Engineers 26918 Hall, Tex G., President, National Congress of American Indians, and Chair man, Mandan, Hidatsa and Arikara Nation 26950 Raley, Bennett, Assistant Secretary, Department of the Interior 2695 Uccellini, Dr. Louis, Director, National Centers for Environmental Prediction, National Oceanic and Atmospheric Administration 26926 APPENDIX Responses to additional questions 2620 67 Title: Western water supply : hearing before the Committee on Energy and Natural Resources, United States Senate, One Hundred Eighth Congress, second session, to receive testimony regarding water supply issues in the arid West, March 9, 2004 Author: United States. Congress. Senate. Committee on Energy and Natural Resources Year: 2004, 2005 CONTENTS STATEMENTS Page American Farm Bureau Federation 26963 Bell, Craig, Executive Director, Western States Water Council 26945 Domenici, Hon. Pete V., U.S. Senator From New Mexico 2691 Gaibler, Floyd, Deputy Undersecretary for Farm and Foreign Agricultural Services, Department of Agriculture 26932 Grisoli, Brigadier General William T., Commander, Northwestern Division, U.S. Army Corps of Engineers 26918 Hall, Tex G., President, National Congress of American Indians, and Chair man, Mandan, Hidatsa and Arikara Nation 26950 Raley, Bennett, Assistant Secretary, Department of the Interior 2695 Uccellini, Dr. Louis, Director, National Centers for Environmental Prediction, National Oceanic and Atmospheric Administration 26926 APPENDIX Responses to additional questions 2620 67

1546. [Image] Handbook for developing watershed plans to restore and protect our waters


	Draft; Title from title screen (viewed on Mar. 17, 2006); "October 2005."; "EPA 841-B-05-005."; Includes bibliographical references
	Citation Citation Citation Abstract Copy Title: Handbook for developing watershed plans to restore and protect our waters Author: United States Environmental Protection Agency, Office of Water Year: 2005, 2008, 2006 Draft; Title from title screen (viewed on Mar. 17, 2006); "October 2005."; "EPA 841-B-05-005."; Includes bibliographical references Title: Handbook for developing watershed plans to restore and protect our waters Author: United States Environmental Protection Agency, Office of Water Year: 2005, 2008, 2006 Draft; Title from title screen (viewed on Mar. 17, 2006); "October 2005."; "EPA 841-B-05-005."; Includes bibliographical references

1547. [Image] Distribution and biology of suckers in Lower Klamath reservoirs : 1999 final report


	Abstract The objectives of this two-year study (1998-1999) were to document distribution, abundance, age class structure, recruitment success, and habitat use by all life history stages of shortnose and ...
	Citation Citation Citation Abstract Copy Title: Distribution and biology of suckers in Lower Klamath reservoirs : 1999 final report Author: Desjardins, Marc; Markle, Douglas F. Year: 2000, 2005 Abstract The objectives of this two-year study (1998-1999) were to document distribution, abundance, age class structure, recruitment success, and habitat use by all life history stages of shortnose and Lost River suckers in three lower Klamath River hydroelectric reservoirs (J. C. Boyle, Copco, and Iron Gate). Lost River sucker catches were sporadic (only 3 adult individuals total) and the focus of our analyses, therefore, shifted to shortnose suckers. Adult and larval suckers were found in all reservoirs both years. All life history stages (larvae, juveniles and adults) were found in J. C. Boyle during both years and in Copco in 1999. Juvenile suckers were not found in Copco in 1998. The number of adult shortnose suckers was highest in Copco reservoir (n=165), followed by J.C. Boyle (n=50) and Iron Gate (n=22). Larger and older individuals dominated Copco and Iron Gate reservoirs and little size structure was detected. J. C. Boyle tended to have smaller adult shortnose suckers and many size classes were present. Unidentifiable larval suckers were most abundant in Copco reservoir where historic spawning of shortnose suckers has been documented. Larval suckers in Copco and Iron Gate reservoirs were most abundant in mid to late June before quickly disappearing from catches. J. C. Boyle larval suckers peaked in mid July, attained larger sizes, and were caught later in the season. It appeared that recruitment of young-of-the-year suckers only occurred in J. C. Boyle with downstream reservoirs recruiting older individuals, perhaps those that had earlier recruited to J. C. Boyle. Tagging studies could clarify adult recruitment dynamics and an additional study of juvenile recruitment would be needed to confirm these patterns. Predation pressure may be somewhat reduced in J. C. Boyle in comparison to the other reservoirs as its fish community was dominated by native fishes while communities in Copco and Iron Gate reservoirs were dominated by exotic predators. J. C. Boyle also possessed proportionally more littoral habitat, which suggests it may provide a more stable environment for young fishes. However, our sampling was inadequate to demonstrate such relationships due to high variance in larval and juvenile catches and potentially confounding habitat variables. One such variable was water level fluctuations, which could interact with habitat and resource availability in complex ways. For example, water level fluctuations, presumed to have a negative impact, were greatest in J. C. Boyle. Extrapolation from the literature suggests it should have had the poorest habitat for larval and juvenile suckers, but our results indicated J. C. Boyle had the most young suckers. Additional study of the relationships between water level fluctuations, habitat availability, the exotic fish community, and juvenile sucker recruitment would be needed to better understand early life history ecology of endangered lake suckers in these systems. Title: Distribution and biology of suckers in Lower Klamath reservoirs : 1999 final report Author: Desjardins, Marc; Markle, Douglas F. Year: 2000, 2005 Abstract The objectives of this two-year study (1998-1999) were to document distribution, abundance, age class structure, recruitment success, and habitat use by all life history stages of shortnose and Lost River suckers in three lower Klamath River hydroelectric reservoirs (J. C. Boyle, Copco, and Iron Gate). Lost River sucker catches were sporadic (only 3 adult individuals total) and the focus of our analyses, therefore, shifted to shortnose suckers. Adult and larval suckers were found in all reservoirs both years. All life history stages (larvae, juveniles and adults) were found in J. C. Boyle during both years and in Copco in 1999. Juvenile suckers were not found in Copco in 1998. The number of adult shortnose suckers was highest in Copco reservoir (n=165), followed by J.C. Boyle (n=50) and Iron Gate (n=22). Larger and older individuals dominated Copco and Iron Gate reservoirs and little size structure was detected. J. C. Boyle tended to have smaller adult shortnose suckers and many size classes were present. Unidentifiable larval suckers were most abundant in Copco reservoir where historic spawning of shortnose suckers has been documented. Larval suckers in Copco and Iron Gate reservoirs were most abundant in mid to late June before quickly disappearing from catches. J. C. Boyle larval suckers peaked in mid July, attained larger sizes, and were caught later in the season. It appeared that recruitment of young-of-the-year suckers only occurred in J. C. Boyle with downstream reservoirs recruiting older individuals, perhaps those that had earlier recruited to J. C. Boyle. Tagging studies could clarify adult recruitment dynamics and an additional study of juvenile recruitment would be needed to confirm these patterns. Predation pressure may be somewhat reduced in J. C. Boyle in comparison to the other reservoirs as its fish community was dominated by native fishes while communities in Copco and Iron Gate reservoirs were dominated by exotic predators. J. C. Boyle also possessed proportionally more littoral habitat, which suggests it may provide a more stable environment for young fishes. However, our sampling was inadequate to demonstrate such relationships due to high variance in larval and juvenile catches and potentially confounding habitat variables. One such variable was water level fluctuations, which could interact with habitat and resource availability in complex ways. For example, water level fluctuations, presumed to have a negative impact, were greatest in J. C. Boyle. Extrapolation from the literature suggests it should have had the poorest habitat for larval and juvenile suckers, but our results indicated J. C. Boyle had the most young suckers. Additional study of the relationships between water level fluctuations, habitat availability, the exotic fish community, and juvenile sucker recruitment would be needed to better understand early life history ecology of endangered lake suckers in these systems.

1548. [Image] Natural history and ecology of larval Lost River suckers and larval shortnose suckers in the Williamson River-Upper Klamath Lake System


	We monitored larval Lost River and shortnose suckers from natal beds in the Williamson and Sprague rivers to nursery grounds in Upper Klamath Lake. Downstream movements occurred at night, in the middle ...
	Citation Citation Citation Abstract Copy Title: Natural history and ecology of larval Lost River suckers and larval shortnose suckers in the Williamson River-Upper Klamath Lake System Author: Cooperman, Michael S. Year: 2004, 2005 We monitored larval Lost River and shortnose suckers from natal beds in the Williamson and Sprague rivers to nursery grounds in Upper Klamath Lake. Downstream movements occurred at night, in the middle of the channel, and on the falling limb of the hydrograph. Ages, sizes, and developmental stages of larvae from spawning beds and the river mouth were similar, while larvae collected contemporaneously from the lake tended to be larger and better fed. Our results indicate in-river rearing was rare, that a rapid outmigration to the lake was favorable for larval survival, and that modification of the lower Williamson River does not appear to have prohibited rapid entry or preclude access to Upper Klamath Lake. Within the Williamson River and Upper Klamath Lake, emergent macrophytes supported significantly higher abundance, larger mean sizes, and better fed larvae than submerged macrophytes, woody vegetation, or open water areas. Analysis of seven years of larval sucker production and survival corroborated the habitat analysis by identifying a positive relationship with emergent macrophyte availability as well as a positive relationship with air temperature and a negative relationship with high wind. These findings illustrate the importance of fast growth, appropriate habitat and calm hydrological conditions for larvae, and are highly consistent with other larval fish studies. Title: Natural history and ecology of larval Lost River suckers and larval shortnose suckers in the Williamson River-Upper Klamath Lake System Author: Cooperman, Michael S. Year: 2004, 2005 We monitored larval Lost River and shortnose suckers from natal beds in the Williamson and Sprague rivers to nursery grounds in Upper Klamath Lake. Downstream movements occurred at night, in the middle of the channel, and on the falling limb of the hydrograph. Ages, sizes, and developmental stages of larvae from spawning beds and the river mouth were similar, while larvae collected contemporaneously from the lake tended to be larger and better fed. Our results indicate in-river rearing was rare, that a rapid outmigration to the lake was favorable for larval survival, and that modification of the lower Williamson River does not appear to have prohibited rapid entry or preclude access to Upper Klamath Lake. Within the Williamson River and Upper Klamath Lake, emergent macrophytes supported significantly higher abundance, larger mean sizes, and better fed larvae than submerged macrophytes, woody vegetation, or open water areas. Analysis of seven years of larval sucker production and survival corroborated the habitat analysis by identifying a positive relationship with emergent macrophyte availability as well as a positive relationship with air temperature and a negative relationship with high wind. These findings illustrate the importance of fast growth, appropriate habitat and calm hydrological conditions for larvae, and are highly consistent with other larval fish studies.

1549. [Image] Klamath Project : hearing before the Subcommittee on Water and Power of the Committee on Energy and Natural Resources, United States Senate, One Hundred Seventh Congress, first session to discuss Klamath Project operations and implementation of Public Law 106-498, March 21, 2001


	CONTENTS STATEMENTS Page Craig, Hon. Larry E., U.S. Senator from Idaho 2693 Crawford, John, Farmer, on behalf of Klamath Water Users Association, Klamath Falls, OR 26951 Foreman, Allen, Chairman, Klamath ...
	Citation Citation Citation Abstract Copy Title: Klamath Project : hearing before the Subcommittee on Water and Power of the Committee on Energy and Natural Resources, United States Senate, One Hundred Seventh Congress, first session to discuss Klamath Project operations and implementation of Public Law 106-498, March 21, 2001 Author: United States. Congress. Senate. Committee on Energy and Natural Resources. Subcommittee on Water and Power Year: 2001, 2005, 2000 CONTENTS STATEMENTS Page Craig, Hon. Larry E., U.S. Senator from Idaho 2693 Crawford, John, Farmer, on behalf of Klamath Water Users Association, Klamath Falls, OR 26951 Foreman, Allen, Chairman, Klamath Indian Tribes, Chiloquin, OR 26923 Home, Alex J., Ph.D., Professor, Department of Civil and Environmental Engineering, University of California, Berkeley 26955 Marbut, Reed, Intergovernmental Coordinator, Oregon Water Resources De partment, Salem, OR 26931 McDonald, J. William, Acting Commissioner, Bureau of Reclamation, Depart ment of the Interior 2697 Nicholson, Roger, President, Resource Conservancy, Fort Klamath, OR 26939 Smith, Hon. Gordon, U.S. Senator from Oregon 2691 Spain, Glen H., Northwest Regional Director, Pacific Coast Federation of Fishermen's Associations, Eugene, OR 26940 Walden, Hon. Greg, U.S. Representative from Oregon 2693 Wyden, Hon. Ron, U.S. Senator from Oregon 2692 Title: Klamath Project : hearing before the Subcommittee on Water and Power of the Committee on Energy and Natural Resources, United States Senate, One Hundred Seventh Congress, first session to discuss Klamath Project operations and implementation of Public Law 106-498, March 21, 2001 Author: United States. Congress. Senate. Committee on Energy and Natural Resources. Subcommittee on Water and Power Year: 2001, 2005, 2000 CONTENTS STATEMENTS Page Craig, Hon. Larry E., U.S. Senator from Idaho 2693 Crawford, John, Farmer, on behalf of Klamath Water Users Association, Klamath Falls, OR 26951 Foreman, Allen, Chairman, Klamath Indian Tribes, Chiloquin, OR 26923 Home, Alex J., Ph.D., Professor, Department of Civil and Environmental Engineering, University of California, Berkeley 26955 Marbut, Reed, Intergovernmental Coordinator, Oregon Water Resources De partment, Salem, OR 26931 McDonald, J. William, Acting Commissioner, Bureau of Reclamation, Depart ment of the Interior 2697 Nicholson, Roger, President, Resource Conservancy, Fort Klamath, OR 26939 Smith, Hon. Gordon, U.S. Senator from Oregon 2691 Spain, Glen H., Northwest Regional Director, Pacific Coast Federation of Fishermen's Associations, Eugene, OR 26940 Walden, Hon. Greg, U.S. Representative from Oregon 2693 Wyden, Hon. Ron, U.S. Senator from Oregon 2692

1550. [Image] Crater Lake National Park oral history series, Emmett Blanchfield


	ill.; "Interviewed by Stephen R. Mark on March 7, 1995; transcribed by Chris Prout, August 1997." - T.p.
	Citation Citation Citation Abstract Copy Title: Crater Lake National Park oral history series, Emmett Blanchfield Author: Mark, Stephen R. Year: 1995, 2010 ill.; "Interviewed by Stephen R. Mark on March 7, 1995; transcribed by Chris Prout, August 1997." - T.p. Title: Crater Lake National Park oral history series, Emmett Blanchfield Author: Mark, Stephen R. Year: 1995, 2010 ill.; "Interviewed by Stephen R. Mark on March 7, 1995; transcribed by Chris Prout, August 1997." - T.p.

1551. [Image] An assessment of ecosystem components in the interior Columbia Basin and portions of the Klamath and Great Basins [volume 2]


	Abstract Quigley, Thomas M.; Arbelbide, Sylvia J., tech. eds. 1997. An assessment of ecosystem components in the interior Columbia basin and portions of the Klamath and Great Basins: volume 2. Gen. Tech. ...
	Citation Citation Citation Abstract Copy Title: An assessment of ecosystem components in the interior Columbia Basin and portions of the Klamath and Great Basins [volume 2] Author: Quigley, Thomas Milton; Arbelbide, S. J. (Sylvia J.) Year: 1997, 2008, 2005 Abstract Quigley, Thomas M.; Arbelbide, Sylvia J., tech. eds. 1997. An assessment of ecosystem components in the interior Columbia basin and portions of the Klamath and Great Basins: volume 2. Gen. Tech. Rep. PNW-GTR-405. Portland, OR: U.S. Department of Agriculture, Forest Service, Pacific Northwest Research Station. 4 vol. (Quigley, Thomas M., tech. ed.; The Interior Columbia Basin Ecosystem Management Project: Scientific Assessment). The Assessment of Ecosystem Components in the Interior Columbia Basin and Portions of the Klamath and Great Basins provides detailed information about current conditions and trends for the biophysical and social systems within the Basin. This information can be used by land managers to develop broad land management goals and priorities and provides the context for decisions specific to smaller geographic areas. The Assessment area covers about 8 percent of the U.S. land area, 24 percent of the Nations National Forest System lands, 10 percent of the Nations BLM-administered lands, and contains about 1.2 percent of the Nations population. This results in a population density that is less than one-sixth of the U.S. average. The area has experienced recent, rapid population growth and generally has a robust, diverse economy. As compared to historic conditions, the terrestrial, aquatic, forest, and rangeland systems have undergone dramatic changes. Forested landscapes are more susceptible to fire, insect, and disease than under historic conditions. Rangelands are highly susceptible to noxious weed invasion. The disturbance regimes that operate on forest and rangeland have changed substantially, with lethal fires dominating many areas where non-lethal fires were the norm historically. Terrestrial habitats that have experienced the greatest decline include the native grassland, native shrubland, and old forest structures. There are areas within the Assessment area that have higher diversity than others. Aquatic systems are now more fragmented and isolated than historically and the introduction of non-native fish species has complicated current status of native fishes. Core habitat and population centers do remain as building blocks for restoration. Social and economic conditions within the Assessment area vary considerably, depending to a great extent on population, diversity of employment opportunities, and changing demographics. Those counties with the higher population densities and greater diversity of employment opportunities are generally more resilient to economic downturns. This Assessment provides a rich information base, including over 170 mapped themes with associated models and databases, from which future decisions can benefit. Keywords: Columbia basin, biophysical systems, social systems, ecosystem. Title: An assessment of ecosystem components in the interior Columbia Basin and portions of the Klamath and Great Basins [volume 2] Author: Quigley, Thomas Milton; Arbelbide, S. J. (Sylvia J.) Year: 1997, 2008, 2005 Abstract Quigley, Thomas M.; Arbelbide, Sylvia J., tech. eds. 1997. An assessment of ecosystem components in the interior Columbia basin and portions of the Klamath and Great Basins: volume 2. Gen. Tech. Rep. PNW-GTR-405. Portland, OR: U.S. Department of Agriculture, Forest Service, Pacific Northwest Research Station. 4 vol. (Quigley, Thomas M., tech. ed.; The Interior Columbia Basin Ecosystem Management Project: Scientific Assessment). The Assessment of Ecosystem Components in the Interior Columbia Basin and Portions of the Klamath and Great Basins provides detailed information about current conditions and trends for the biophysical and social systems within the Basin. This information can be used by land managers to develop broad land management goals and priorities and provides the context for decisions specific to smaller geographic areas. The Assessment area covers about 8 percent of the U.S. land area, 24 percent of the Nations National Forest System lands, 10 percent of the Nations BLM-administered lands, and contains about 1.2 percent of the Nations population. This results in a population density that is less than one-sixth of the U.S. average. The area has experienced recent, rapid population growth and generally has a robust, diverse economy. As compared to historic conditions, the terrestrial, aquatic, forest, and rangeland systems have undergone dramatic changes. Forested landscapes are more susceptible to fire, insect, and disease than under historic conditions. Rangelands are highly susceptible to noxious weed invasion. The disturbance regimes that operate on forest and rangeland have changed substantially, with lethal fires dominating many areas where non-lethal fires were the norm historically. Terrestrial habitats that have experienced the greatest decline include the native grassland, native shrubland, and old forest structures. There are areas within the Assessment area that have higher diversity than others. Aquatic systems are now more fragmented and isolated than historically and the introduction of non-native fish species has complicated current status of native fishes. Core habitat and population centers do remain as building blocks for restoration. Social and economic conditions within the Assessment area vary considerably, depending to a great extent on population, diversity of employment opportunities, and changing demographics. Those counties with the higher population densities and greater diversity of employment opportunities are generally more resilient to economic downturns. This Assessment provides a rich information base, including over 170 mapped themes with associated models and databases, from which future decisions can benefit. Keywords: Columbia basin, biophysical systems, social systems, ecosystem.

1552. [Image] Water management and endangered species issues in the Klamath Basin : oversight field hearing before the Committee on Resources, U.S. House of Representatives, One Hundred Seventh Congress, first session, June 16, 2001 in Klamath Falls, Oregon


	"Serial no. 107-39."
	Citation Citation Citation Abstract Copy Title: Water management and endangered species issues in the Klamath Basin : oversight field hearing before the Committee on Resources, U.S. House of Representatives, One Hundred Seventh Congress, first session, June 16, 2001 in Klamath Falls, Oregon Author: United States. Congress. House. Committee on Resources Year: 2002, 2005, 2004 "Serial no. 107-39." Title: Water management and endangered species issues in the Klamath Basin : oversight field hearing before the Committee on Resources, U.S. House of Representatives, One Hundred Seventh Congress, first session, June 16, 2001 in Klamath Falls, Oregon Author: United States. Congress. House. Committee on Resources Year: 2002, 2005, 2004 "Serial no. 107-39."

1553. [Image] Soil survey of Klamath County, Oregon, southern part


	Foreword The Soil Survey of Klamath County, Oregon, Southern Part, is the product of many soil scientists, plant specialists, soil engineers, extension specialists, land owners, and others who worked ...
	Citation Citation Citation Abstract Copy Title: Soil survey of Klamath County, Oregon, southern part Author: Cahoon, Joe Year: 1985, 2006, 2005 Foreword The Soil Survey of Klamath County, Oregon, Southern Part, is the product of many soil scientists, plant specialists, soil engineers, extension specialists, land owners, and others who worked and cooperated as a team to complete this project. In this report are many kinds of basic information about the soils in the area. This information can be helpful in making decisions about the management of irrigated soils for optimum crop production, in planning land uses for urban and suburban areas, and in determining the needs for many other uses, for example, forestry, range, wildlife, and recreation. This soil survey has been prepared for many different users. Farmers can use it to help select the most suitable crop for the kind of soil; ranchers can use it to determine amount of forage production and the kinds of plants most suited to range or woodland; foresters can use the survey to find information about kinds of trees, potential for tree growth, and special soil features. Title: Soil survey of Klamath County, Oregon, southern part Author: Cahoon, Joe Year: 1985, 2006, 2005 Foreword The Soil Survey of Klamath County, Oregon, Southern Part, is the product of many soil scientists, plant specialists, soil engineers, extension specialists, land owners, and others who worked and cooperated as a team to complete this project. In this report are many kinds of basic information about the soils in the area. This information can be helpful in making decisions about the management of irrigated soils for optimum crop production, in planning land uses for urban and suburban areas, and in determining the needs for many other uses, for example, forestry, range, wildlife, and recreation. This soil survey has been prepared for many different users. Farmers can use it to help select the most suitable crop for the kind of soil; ranchers can use it to determine amount of forage production and the kinds of plants most suited to range or woodland; foresters can use the survey to find information about kinds of trees, potential for tree growth, and special soil features.

1554. [Image] Anomalies of larval and juvenile shortnose and Lost River suckers in Upper Klamath Lake, Oregon


	Abstract-Larval and juvenile shortnose {Chasmistes brevirostris) and Lost River (Deltistes luxatus) suckers from Upper Klamath Lake, OR, were examined to determine anomaly rates for fins, eyes, spinal ...
	Citation Citation Citation Abstract Copy Title: Anomalies of larval and juvenile shortnose and Lost River suckers in Upper Klamath Lake, Oregon Author: Plunkett, Steven R.; Snyder-Conn, Elaine Year: 2000, 2005 Abstract-Larval and juvenile shortnose {Chasmistes brevirostris) and Lost River (Deltistes luxatus) suckers from Upper Klamath Lake, OR, were examined to determine anomaly rates for fins, eyes, spinal column, vertebrae, and osteocranium, and their possible associations with water quality and pesticides. X-rays of 1,550 fish and 1,395 matching specimens, collected in 1993, were ranked on the severity of anomalies. One or more anomalies were observed in 15.9% of shortnose suckers and 8.2% of Lost River suckers. Anomaly rates exceeding 1.0%, greater than rates expected from high water quality systems, were observed for lordosis and scoliosis, and abnormalities of the vertebrae, opercula, and pectoral and pelvic fins in shortnose suckers, and abnormalities of vertebrae and opercula in Lost River suckers. The highest rates of anomalies were in vertebrae, pelvic fins, and opercula in shortnose suckers, and opercula and vertebrae in Lost River suckers. Shortnose suckers exhibited higher rates than Lost River suckers for almost all anomalies. Particular anomaly rates differed significantly among sites. There were also substantially more anomalies found in larvae and small juveniles than in larger juveniles. Based on the high anomaly rates observed in this study, it is possible that 0-aged sucker cohorts in Upper Klamath Lake are far more vulnerable to mortality. Title: Anomalies of larval and juvenile shortnose and Lost River suckers in Upper Klamath Lake, Oregon Author: Plunkett, Steven R.; Snyder-Conn, Elaine Year: 2000, 2005 Abstract-Larval and juvenile shortnose {Chasmistes brevirostris) and Lost River (Deltistes luxatus) suckers from Upper Klamath Lake, OR, were examined to determine anomaly rates for fins, eyes, spinal column, vertebrae, and osteocranium, and their possible associations with water quality and pesticides. X-rays of 1,550 fish and 1,395 matching specimens, collected in 1993, were ranked on the severity of anomalies. One or more anomalies were observed in 15.9% of shortnose suckers and 8.2% of Lost River suckers. Anomaly rates exceeding 1.0%, greater than rates expected from high water quality systems, were observed for lordosis and scoliosis, and abnormalities of the vertebrae, opercula, and pectoral and pelvic fins in shortnose suckers, and abnormalities of vertebrae and opercula in Lost River suckers. The highest rates of anomalies were in vertebrae, pelvic fins, and opercula in shortnose suckers, and opercula and vertebrae in Lost River suckers. Shortnose suckers exhibited higher rates than Lost River suckers for almost all anomalies. Particular anomaly rates differed significantly among sites. There were also substantially more anomalies found in larvae and small juveniles than in larger juveniles. Based on the high anomaly rates observed in this study, it is possible that 0-aged sucker cohorts in Upper Klamath Lake are far more vulnerable to mortality.

1555. [Image] Hydrogeology and paleohydrology in the Williamson River basin, Klamath County, Oregon


	Abstract An abstract of the thesis of Jeffrey Scott Conaway for the Master of Science in Geology presented December 8, 1999. Title: Hydrogeology and Paleohydrology in the Williamson River Basin, Klamath ...
	Citation Citation Citation Abstract Copy Title: Hydrogeology and paleohydrology in the Williamson River basin, Klamath County, Oregon Author: Conaway, Jeffrey Scott Year: 2000, 2008, 2005 Abstract An abstract of the thesis of Jeffrey Scott Conaway for the Master of Science in Geology presented December 8, 1999. Title: Hydrogeology and Paleohydrology in the Williamson River Basin, Klamath County, Oregon. Stress on the water resources of the Williamson River basin has led to their regulation to protect important habitat. Quantification of this resource is required for accurate regulation. A portion of this study is a hydrogeologic reconnaissance that suggests directions for future work. Measured discharge and deuterium isotope data from points above and below the Williamson River canyon indicate that the river receives 99% of its discharge from ground water during periods of low flow. The principle aquifer of the southern Klamath Marsh is a fractured basalt, while continental sediments that are up to 200 m thick provide high artesian yields south of the canyon. The disparity between high precipitation on the basin's western margin and the low and variable discharge of the Williamson River at the Kirk Sill suggests either the presence of a fault zone that interrupts the flow of ground water or deep flow paths that do not surface within Klamath Marsh. Three terraces line the eastern edge of Klamath Marsh at approximate elevations of 1380, 1385, and 1397 m. The lowest terrace is late Holocene and cut into marsh sediment and reworked deposits from the pyroclastic eruptions of Mount Mazama. The middle terrace is planed into bedrock and formed when Pleistocene Lake Chemult occupied this basin. The upper terrace, a strand line, is delineated by a slope break that separates reworked pyroclastic deposits from undisturbed pyroclastic fall. Formation of this terrace occurred when pyroclastic flows from the cataclysmic eruption of Mount Mazama formed a blockage in the Williamson River canyon. Resultant backflooding reworked pyroclastic deposits and rafted pumice up to an approximate elevation of 1400 m. The blockage failed catastrophically from overtopping, draining 5.7 x 109 m3 of water, scouring the canyon and producing an erratic boulder deposit at the mouth of the canyon. Upstream evidence of rapid draining includes linear scour channels incised in pyroclastic-flow deposits and scouring of the broad Pleistocene terrace. Paleohydraulic reconstruction of down stream flooding using a flow-competence equation and a physically based dam-break model yield a peak discharge of 1.3 x 104 m3 s"1. Title: Hydrogeology and paleohydrology in the Williamson River basin, Klamath County, Oregon Author: Conaway, Jeffrey Scott Year: 2000, 2008, 2005 Abstract An abstract of the thesis of Jeffrey Scott Conaway for the Master of Science in Geology presented December 8, 1999. Title: Hydrogeology and Paleohydrology in the Williamson River Basin, Klamath County, Oregon. Stress on the water resources of the Williamson River basin has led to their regulation to protect important habitat. Quantification of this resource is required for accurate regulation. A portion of this study is a hydrogeologic reconnaissance that suggests directions for future work. Measured discharge and deuterium isotope data from points above and below the Williamson River canyon indicate that the river receives 99% of its discharge from ground water during periods of low flow. The principle aquifer of the southern Klamath Marsh is a fractured basalt, while continental sediments that are up to 200 m thick provide high artesian yields south of the canyon. The disparity between high precipitation on the basin's western margin and the low and variable discharge of the Williamson River at the Kirk Sill suggests either the presence of a fault zone that interrupts the flow of ground water or deep flow paths that do not surface within Klamath Marsh. Three terraces line the eastern edge of Klamath Marsh at approximate elevations of 1380, 1385, and 1397 m. The lowest terrace is late Holocene and cut into marsh sediment and reworked deposits from the pyroclastic eruptions of Mount Mazama. The middle terrace is planed into bedrock and formed when Pleistocene Lake Chemult occupied this basin. The upper terrace, a strand line, is delineated by a slope break that separates reworked pyroclastic deposits from undisturbed pyroclastic fall. Formation of this terrace occurred when pyroclastic flows from the cataclysmic eruption of Mount Mazama formed a blockage in the Williamson River canyon. Resultant backflooding reworked pyroclastic deposits and rafted pumice up to an approximate elevation of 1400 m. The blockage failed catastrophically from overtopping, draining 5.7 x 109 m3 of water, scouring the canyon and producing an erratic boulder deposit at the mouth of the canyon. Upstream evidence of rapid draining includes linear scour channels incised in pyroclastic-flow deposits and scouring of the broad Pleistocene terrace. Paleohydraulic reconstruction of down stream flooding using a flow-competence equation and a physically based dam-break model yield a peak discharge of 1.3 x 104 m3 s"1.

1556. [Image] Report of 1994 Workshop on the Correlation of Marine and Terrestrial Records of Climate Changes in the Western United States


	Imprint from transmittal sheet; Distributed to depository libraries in microfiche; Shipping list no.: 97-0071-M; One ill. on 1 folded leaf in pocket; Includes bibliographical references
	Citation Citation Citation Abstract Copy Title: Report of 1994 Workshop on the Correlation of Marine and Terrestrial Records of Climate Changes in the Western United States Author: Workshop on the Correlation of Marine and Terrestrial Records of Climate Changes in the Western U.S. (3rd : 1994 : Watsonville, Calif.) Year: 1996, 2007, 2005 Imprint from transmittal sheet; Distributed to depository libraries in microfiche; Shipping list no.: 97-0071-M; One ill. on 1 folded leaf in pocket; Includes bibliographical references Title: Report of 1994 Workshop on the Correlation of Marine and Terrestrial Records of Climate Changes in the Western United States Author: Workshop on the Correlation of Marine and Terrestrial Records of Climate Changes in the Western U.S. (3rd : 1994 : Watsonville, Calif.) Year: 1996, 2007, 2005 Imprint from transmittal sheet; Distributed to depository libraries in microfiche; Shipping list no.: 97-0071-M; One ill. on 1 folded leaf in pocket; Includes bibliographical references

1557. [Image] Final supplemental environmental impact statement: for clarification of language in the 1994 record of decision for the Northwest Forest Plan; national forests and Bureau of Land Management districts within the range of the northern spotted owl: proposal to amend wording about the aquatic conservation strategy


	Abstract The Secretaries of Agriculture and the Interior propose limited changes to language about how to demonstrate that projects follow the Aquatic Conservation Strategy, part of the Northwest Forest ...
	Citation Citation Citation Abstract Copy Title: Final supplemental environmental impact statement: for clarification of language in the 1994 record of decision for the Northwest Forest Plan; national forests and Bureau of Land Management districts within the range of the northern spotted owl: proposal to amend wording about the aquatic conservation strategy Author: United States. Department of Agriculture. Forest Service; United States. Department of the Interior. Bureau of Land Managemen Year: 2003, 2006, 2005 Abstract The Secretaries of Agriculture and the Interior propose limited changes to language about how to demonstrate that projects follow the Aquatic Conservation Strategy, part of the Northwest Forest Plan. Projects needed to achieve Northwest Forest Plan goals have been delayed or stopped due to misapplication of certain passages in the Aquatic Conservation Strategy. The agencies are responding to the underlying need for increased agency success planning and implementing projects, to the extent that the current wording has hindered the agencies ability to follow Northwest Forest Plan principles and achieve its goals. The goals of the Northwest Forest Plan cannot be achieved without project implementation. Three alternatives are considered in the Final Supplemental Environmental Impact Statement, No Action, the Proposed Action, and Alternative A. No Action would not change existing language within the Aquatic Conservation Strategy. The Proposed Action and Alternative A would make l Title: Final supplemental environmental impact statement: for clarification of language in the 1994 record of decision for the Northwest Forest Plan; national forests and Bureau of Land Management districts within the range of the northern spotted owl: proposal to amend wording about the aquatic conservation strategy Author: United States. Department of Agriculture. Forest Service; United States. Department of the Interior. Bureau of Land Managemen Year: 2003, 2006, 2005 Abstract The Secretaries of Agriculture and the Interior propose limited changes to language about how to demonstrate that projects follow the Aquatic Conservation Strategy, part of the Northwest Forest Plan. Projects needed to achieve Northwest Forest Plan goals have been delayed or stopped due to misapplication of certain passages in the Aquatic Conservation Strategy. The agencies are responding to the underlying need for increased agency success planning and implementing projects, to the extent that the current wording has hindered the agencies ability to follow Northwest Forest Plan principles and achieve its goals. The goals of the Northwest Forest Plan cannot be achieved without project implementation. Three alternatives are considered in the Final Supplemental Environmental Impact Statement, No Action, the Proposed Action, and Alternative A. No Action would not change existing language within the Aquatic Conservation Strategy. The Proposed Action and Alternative A would make l

1558. [Image] An examination of the Klamath Basin crisis : restructuring the discourse within an identity-based framework


	Thesis (B.A.) -- Whitman College, 2002; Includes bibliographical references (leaves 79-83)
	Citation Citation Citation Abstract Copy Title: An examination of the Klamath Basin crisis : restructuring the discourse within an identity-based framework Author: Dornsife, Alison M. Year: 2002, 2005, 2004 Thesis (B.A.) -- Whitman College, 2002; Includes bibliographical references (leaves 79-83) Title: An examination of the Klamath Basin crisis : restructuring the discourse within an identity-based framework Author: Dornsife, Alison M. Year: 2002, 2005, 2004 Thesis (B.A.) -- Whitman College, 2002; Includes bibliographical references (leaves 79-83)

1559. [Image] Annual project history and O. & M. report of the Klamath Project, Oregon-California, 1918


	Ill., maps (some color), photographs; Includes fiscal year financials and contracts, land acquired, land leased, project organization chart, litigations, photographs, maps, hydrographs, etc.; Includes ...
	Citation Citation Citation Abstract Copy Title: Annual project history and O. & M. report of the Klamath Project, Oregon-California, 1918 Author: United States. Bureau of Reclamation Year: 1918, 2008, 2004 Ill., maps (some color), photographs; Includes fiscal year financials and contracts, land acquired, land leased, project organization chart, litigations, photographs, maps, hydrographs, etc.; Includes index; Title covers: calendar years for 1918 – 1943; Description based on Annual project history and O.M. report of the Klamath Project, Oregon-California Annual for calendar year 1918; Dates of the beginning year(s) of publication are derived from the 1903 to December 31, 1912, History of the Klamath Project and from the volume information on later volumes (v. 35) Klamath District and Klamath Project annual history for 1945, dated December 1, 1946 Title: Annual project history and O. & M. report of the Klamath Project, Oregon-California, 1918 Author: United States. Bureau of Reclamation Year: 1918, 2008, 2004 Ill., maps (some color), photographs; Includes fiscal year financials and contracts, land acquired, land leased, project organization chart, litigations, photographs, maps, hydrographs, etc.; Includes index; Title covers: calendar years for 1918 – 1943; Description based on Annual project history and O.M. report of the Klamath Project, Oregon-California Annual for calendar year 1918; Dates of the beginning year(s) of publication are derived from the 1903 to December 31, 1912, History of the Klamath Project and from the volume information on later volumes (v. 35) Klamath District and Klamath Project annual history for 1945, dated December 1, 1946

1560. [Image] Annual report of the Klamath Project, Oregon-California, 1917


	Photographs, maps, and tables for land acquired, hydrographs, contracts, etc.; Description based on Annual Report of the Klamath project: Oregon and California for calendar year 1914; Title covers: calendar ...
	Citation Citation Citation Abstract Copy Title: Annual report of the Klamath Project, Oregon-California, 1917 Author: United States. Bureau of Reclamation Year: 1917, 2008, 2005 Photographs, maps, and tables for land acquired, hydrographs, contracts, etc.; Description based on Annual Report of the Klamath project: Oregon and California for calendar year 1914; Title covers: calendar years for 1913 - 1917; Dates of the beginning year(s) of publication are derived from the 1903 to December 31, 1912, History of the Klamath Project and from the volume information on later volumes (v. 35) Klamath District and Klamath Title: Annual report of the Klamath Project, Oregon-California, 1917 Author: United States. Bureau of Reclamation Year: 1917, 2008, 2005 Photographs, maps, and tables for land acquired, hydrographs, contracts, etc.; Description based on Annual Report of the Klamath project: Oregon and California for calendar year 1914; Title covers: calendar years for 1913 - 1917; Dates of the beginning year(s) of publication are derived from the 1903 to December 31, 1912, History of the Klamath Project and from the volume information on later volumes (v. 35) Klamath District and Klamath

1561. [Image] The Bull trout (salvelinus confluentus) population within Crater Lake National Park: summarized information relating to its conservation and perpetuation


	ill.,; Report title; "On October 7 and 8, 1991 an advisory panel\recovery team met at Crater Lake National Park to review the status of the park's only native fish population, and to develop recommendations ...
	Citation Citation Citation Abstract Copy Title: The Bull trout (salvelinus confluentus) population within Crater Lake National Park: summarized information relating to its conservation and perpetuation Author: Pister, Edwin P. Year: 1992, 2010 ill.,; Report title; "On October 7 and 8, 1991 an advisory panel\recovery team met at Crater Lake National Park to review the status of the park's only native fish population, and to develop recommendations for a recovery program to restore the Sun Creek Bull Trout population to historic range and abundance within Crater Lake National Park." - P. [ii].; Title: The Bull trout (salvelinus confluentus) population within Crater Lake National Park: summarized information relating to its conservation and perpetuation Author: Pister, Edwin P. Year: 1992, 2010 ill.,; Report title; "On October 7 and 8, 1991 an advisory panel\recovery team met at Crater Lake National Park to review the status of the park's only native fish population, and to develop recommendations for a recovery program to restore the Sun Creek Bull Trout population to historic range and abundance within Crater Lake National Park." - P. [ii].;

1562. [Image] Bull trout restoration and brook trout eradication at Crater Lake National Park, Oregon


	ill., 1 map (sketched) ; Report title; "Drought conditions are continuing in 1994, at the writing of this report in March of 1994, Crater Lake National Park had received approximately 50% of the annual ...
	Citation Citation Citation Abstract Copy Title: Bull trout restoration and brook trout eradication at Crater Lake National Park, Oregon Author: Buktenica, Mark. Year: 1994, 2008, 2009 ill., 1 map (sketched) ; Report title; "Drought conditions are continuing in 1994, at the writing of this report in March of 1994, Crater Lake National Park had received approximately 50% of the annual average accumulated precipatation to date." - P. 17.; Title: Bull trout restoration and brook trout eradication at Crater Lake National Park, Oregon Author: Buktenica, Mark. Year: 1994, 2008, 2009 ill., 1 map (sketched) ; Report title; "Drought conditions are continuing in 1994, at the writing of this report in March of 1994, Crater Lake National Park had received approximately 50% of the annual average accumulated precipatation to date." - P. 17.;

1563. [Image] A framework for ecosystem management in the interior Columbia Basin and portions of the Klamath and Great Basins


	Haynes, Richard W.; Graham, Russell T.; Quigley, Thomas M., tech. eds. 1996. A framework for ecosystem management in the Interior Columbia Basin including portions of the Klamath and Great Basins. Gen. ...
	Citation Citation Citation Abstract Copy Title: A framework for ecosystem management in the interior Columbia Basin and portions of the Klamath and Great Basins Year: 1996, 2005 Haynes, Richard W.; Graham, Russell T.; Quigley, Thomas M., tech. eds. 1996. A framework for ecosystem management in the Interior Columbia Basin including portions of the Klamath and Great Basins. Gen. Tech. Rep. PNW-GTR-374. Portland, OR; U.S. Department of Agriculture, Forest Service, Pacific Northwest Research Station. 66 p. A framework for ecosystem management is proposed. This framework assumes the purpose of ecosystem management is to maintain the integrity of ecosystems over time and space. It is based on four ecosystem principles: ecosystems are dynamic, can be viewed as hierarchies with temporal and spatial dimensions, have limits, and are relatively unpredictable. This approach recognizes that people are part of ecosystems and that stewardship must be able to resolve tough challenges including how to meet multiple demands with finite resources. The framework describes a general planning model for ecosystem management that has four iterative steps: monitoring, assessment, decision-making, and implementation. Since ecosystems cross jurisdictional lines, the implementation of the framework depends on partnerships among land managers, the scientific community, and stakeholders. It proposes that decision-making be based on information provided by the best available science and the most appropriate technologies for land management. Keywords: Ecosystem assessment, ecosystem principles, ecosystem management, planning models, management goals, risk analysis. Title: A framework for ecosystem management in the interior Columbia Basin and portions of the Klamath and Great Basins Year: 1996, 2005 Haynes, Richard W.; Graham, Russell T.; Quigley, Thomas M., tech. eds. 1996. A framework for ecosystem management in the Interior Columbia Basin including portions of the Klamath and Great Basins. Gen. Tech. Rep. PNW-GTR-374. Portland, OR; U.S. Department of Agriculture, Forest Service, Pacific Northwest Research Station. 66 p. A framework for ecosystem management is proposed. This framework assumes the purpose of ecosystem management is to maintain the integrity of ecosystems over time and space. It is based on four ecosystem principles: ecosystems are dynamic, can be viewed as hierarchies with temporal and spatial dimensions, have limits, and are relatively unpredictable. This approach recognizes that people are part of ecosystems and that stewardship must be able to resolve tough challenges including how to meet multiple demands with finite resources. The framework describes a general planning model for ecosystem management that has four iterative steps: monitoring, assessment, decision-making, and implementation. Since ecosystems cross jurisdictional lines, the implementation of the framework depends on partnerships among land managers, the scientific community, and stakeholders. It proposes that decision-making be based on information provided by the best available science and the most appropriate technologies for land management. Keywords: Ecosystem assessment, ecosystem principles, ecosystem management, planning models, management goals, risk analysis.

1564. [Image] Bull Trout, Salvelinus Confluentus... Draft Recovery Plan, Chapter 2, Klamath River Recovery Unit...U.S. Department Of The Interior


	KLAMATH RIVER RECOVERY UNIT CHAPTER OF THE BULL TROUT RECOVERY PLAN EXECUTIVE SUMMARY CURRENT SPECIES STATUS Klamath River bull trout were listed as a distinct population segment ...
	Citation Citation Citation Abstract Copy Title: Bull Trout, Salvelinus Confluentus... Draft Recovery Plan, Chapter 2, Klamath River Recovery Unit...U.S. Department Of The Interior Year: 2008, 2005 KLAMATH RIVER RECOVERY UNIT CHAPTER OF THE BULL TROUT RECOVERY PLAN EXECUTIVE SUMMARY CURRENT SPECIES STATUS Klamath River bull trout were listed as a distinct population segment in 1998 (63 FR 31647) because they are physically isolated from other bull trout by the Pacific Ocean and several small mountain ranges in central Oregon. Recovery of bull trout in the Klamath River Recovery Unit, which includes three core areas and nine currently identified local populations, will require cooperation from Federal, State, and local agencies, and Tribal and private entities. Within the Klamath River Recovery Unit, abundance has been severely reduced and remaining populations are fragmented. HABITAT REQUIREMENTS AND LIMITING FACTORS Watershed disruption has played a major role in the decline of bull trout in the Klamath River basin. The effects of historical land use on fish habitat in the larger tributaries and mainstem rivers of the Klamath River basin have been profound. Channelization, water withdrawals, removal of streamside vegetation, and other disturbances have altered the aquatic environment by elevating water temperatures, reducing water quantity and quality, and increasing sedimentation. Changes in or disruptions to watershed processes that influence characteristics of stream channels have also influenced the dynamics and persistence of bull trout populations. Klamath River basin bull trout are threatened by habitat degradation, past and present land use management practices, agricultural water diversions, and competition or hybridization from normative brown and brook trout. As a result of past land and resource management practices, bull trout populations in the Klamath River Recovery Unit are small, disjunct, and face a high risk of extirpation. IV RECOVERY GOAL AND OBJECTIVES The goal of the bull trout recovery plan is to ensure the long-term persistence of self-sustaining, complex interacting groups of bull trout distributed across the species range, so that the species can be delisted. In order to recover bull trout in the Klamath River, the following objectives need to be met: ? Maintain current distribution of bull trout and restore distribution in previously occupied areas within the Klamath River Recovery Unit, as noted in Appendix A. ? Maintain stable or increasing trends in abundance of bull trout within the Klamath River. This objective includes the expression of all life history strategies including resident, fluvial, and adfluvial forms in the Upper Klamath Lake core area and resident and fluvial forms in the Sycan River and Upper Sprague River core areas. ? Restore and maintain suitable habitat conditions for all bull trout life history stages and strategies. In core areas and migration corridors, stable or upward trends in habitat quality are achieved through landscape-level adjustments in land management strategies designed to maintain and/or enhance structural and functional attributes of upslope, riparian, and fluvial systems. ? Conserve genetic diversity and provide opportunity for interchange of genetic material among appropriate core populations. RECOVERY CRITERIA Recovery criteria for the Klamath River Recovery Unit reflect the stated objectives and consideration of population and habitat characteristics within the recovery unit. Using four population and habitat elements, the Klamath River Recovery Unit Team categorized bull trout into three groups of relative risk: diminished, intermediate, and increased. Team members evaluated bull trout under current and potential recovered conditions based on the number of local populations, adult abundance, population trends and variability, and connectivity of the system. These elements were derived from the best scientific information available concerning bull trout population and habitat requirements. Evaluation of these elements under a recovered condition assumed that actions identified within this chapter had been implemented. 1. Distribution criteria will be met when current distribution of bull trout in the 12 local populations is maintained and distribution is expanded by establishing bull trout in areas identified as suitable for potential local populations. The number of existing local populations by core area are as follows: Upper Klamath Lake, 3; Sycan River, 2; and Upper Sprague River, 7. Achieving criterion 1 entails maintaining existing local populations and establishing additional potential local populations in all core areas in the recovery unit to maintain current and recovered distribution. To achieve criterion 1 and to ensure a core area population of no fewer than 100 adult bull trout, establishing at least 5 to 7 local populations in the Klamath Lake core area among 15 potential local populations (2 to 5 new local populations), at least 5 to 7 local populations in the Sycan River core area from among 15 potential local populations (3 to 5 new local populations), and at least 10 to 12 local populations in the Upper Sprague River core area from among 25 potential local populations (3 to 5 new local populations) is necessary. 2. Abundance criteria will be met when the estimated number of adult bull trout is at least 8,250 individuals distributed among the Upper Klamath Lake, Sycan River, and Upper Sprague River core areas, based on 10 years of monitoring data. 3. Trend criteria will be met when adult bull trout exhibit stable or increasing trends in abundance in the Upper Klamath Lake, Sycan River, and Upper Sprague River core areas, based on 2 generations (10 years) of monitoring data. VI 4. Connectivity criteria will be met when specific barriers to bull trout migration in the Klamath River Recovery Unit have been addressed. In the Klamath River Recovery Unit, this objective means addressing passage: 1) existing culverts that impede passage should be replaced, including those on Threemile Creek at U.S. Forest Service Road 110 crossing, Brownsworth Creek at U.S. Forest Service Road 34 crossing, and Brownsworth Creek both 0.75 mile and 1.25 miles above U.S. Forest Service Road 34; the culvert 0.25 mile below U.S. Forest Service Road 34 (to prevent repeated washout); the large-diameter culvert at the Boulder Creek road crossing; culverts in the upper Sycan River watershed that are identified in the Fremont National Forest inventory; and several in the North Fork Sprague River drainage, namely, on North Fork Sprague River (2), Boulder Creek (1), Dead Cow Creek (1), and Sheepy Creek (1); 2) fish passage structures should be installed at water diversions on bull trout streams, and barriers should be removed, including on Cherry, Sevenmile, Sun, and Threemile Creeks; 3) fish screens should be installed to prevent fish from entering diversion canals or pipes, including on Long, Deming, Threemile, Sun, Sevenmile, and Cherry Creeks; 4) manmade barriers and entrainment should be evaluated and remedied to promote migratory bull trout; priority watersheds include Threemile, Long, Deming, Sevenmile, Cherry, Sun, and Long Creeks. The Klamath River Recovery Unit team expects that the recovery process will be dynamic and will be refined as more information becomes available. Future adaptive management will play a major role in recovery implementation and refinement of recovery criteria. The recovery unit criteria listed above will be used to determine when the Klamath River Recovery Unit is fully contributing to recovery of the Klamath River population segment. vn ACTIONS NEEDED Recovery for bull trout will entail reducing threats to the long-term persistence of populations and their habitats, ensuring the security of multiple interacting groups of bull trout, and providing habitat and access to conditions that allow for the expression of various life history forms. The seven categories are listed in Chapter 1; tasks specific to this recovery unit are provided in this chapter. ESTIMATED COST OF RECOVERY Total cost of bull trout recovery in the Klamath River Recovery Unit is estimated at about $26 million spread over a 25-year recovery period. Successful recovery of bull trout in the recovery unit is contingent on removing threats from nonnative species, eliminating barriers to fish movement, and improving habitat conditions within the Klamath River basin. Total cost includes estimates of expenditures by local, Tribal, State, and Federal governments and by private business and individuals. Cost estimates are not provided for tasks which are normal agency responsibilities under existing authorities. The estimated costs are attributed to bull trout conservation, but other aquatic species will also benefit. ESTIMATED DATE OF RECOVERY Time required to achieve recovery depends on bull trout status, factors affecting bull trout, implementation and effectiveness of recovery tasks, and responses to recovery tasks. A tremendous amount of work will be required to restore impaired habitat, reconnect habitat, and eliminate threats from nonnative species. Three to five bull trout generations (15 to 25 years), or possibly longer, may be necessary before identified threats to the species can be significantly reduced and bull trout can be considered eligible for delisting. vin Title: Bull Trout, Salvelinus Confluentus... Draft Recovery Plan, Chapter 2, Klamath River Recovery Unit...U.S. Department Of The Interior Year: 2008, 2005 KLAMATH RIVER RECOVERY UNIT CHAPTER OF THE BULL TROUT RECOVERY PLAN EXECUTIVE SUMMARY CURRENT SPECIES STATUS Klamath River bull trout were listed as a distinct population segment in 1998 (63 FR 31647) because they are physically isolated from other bull trout by the Pacific Ocean and several small mountain ranges in central Oregon. Recovery of bull trout in the Klamath River Recovery Unit, which includes three core areas and nine currently identified local populations, will require cooperation from Federal, State, and local agencies, and Tribal and private entities. Within the Klamath River Recovery Unit, abundance has been severely reduced and remaining populations are fragmented. HABITAT REQUIREMENTS AND LIMITING FACTORS Watershed disruption has played a major role in the decline of bull trout in the Klamath River basin. The effects of historical land use on fish habitat in the larger tributaries and mainstem rivers of the Klamath River basin have been profound. Channelization, water withdrawals, removal of streamside vegetation, and other disturbances have altered the aquatic environment by elevating water temperatures, reducing water quantity and quality, and increasing sedimentation. Changes in or disruptions to watershed processes that influence characteristics of stream channels have also influenced the dynamics and persistence of bull trout populations. Klamath River basin bull trout are threatened by habitat degradation, past and present land use management practices, agricultural water diversions, and competition or hybridization from normative brown and brook trout. As a result of past land and resource management practices, bull trout populations in the Klamath River Recovery Unit are small, disjunct, and face a high risk of extirpation. IV RECOVERY GOAL AND OBJECTIVES The goal of the bull trout recovery plan is to ensure the long-term persistence of self-sustaining, complex interacting groups of bull trout distributed across the species range, so that the species can be delisted. In order to recover bull trout in the Klamath River, the following objectives need to be met: ? Maintain current distribution of bull trout and restore distribution in previously occupied areas within the Klamath River Recovery Unit, as noted in Appendix A. ? Maintain stable or increasing trends in abundance of bull trout within the Klamath River. This objective includes the expression of all life history strategies including resident, fluvial, and adfluvial forms in the Upper Klamath Lake core area and resident and fluvial forms in the Sycan River and Upper Sprague River core areas. ? Restore and maintain suitable habitat conditions for all bull trout life history stages and strategies. In core areas and migration corridors, stable or upward trends in habitat quality are achieved through landscape-level adjustments in land management strategies designed to maintain and/or enhance structural and functional attributes of upslope, riparian, and fluvial systems. ? Conserve genetic diversity and provide opportunity for interchange of genetic material among appropriate core populations. RECOVERY CRITERIA Recovery criteria for the Klamath River Recovery Unit reflect the stated objectives and consideration of population and habitat characteristics within the recovery unit. Using four population and habitat elements, the Klamath River Recovery Unit Team categorized bull trout into three groups of relative risk: diminished, intermediate, and increased. Team members evaluated bull trout under current and potential recovered conditions based on the number of local populations, adult abundance, population trends and variability, and connectivity of the system. These elements were derived from the best scientific information available concerning bull trout population and habitat requirements. Evaluation of these elements under a recovered condition assumed that actions identified within this chapter had been implemented. 1. Distribution criteria will be met when current distribution of bull trout in the 12 local populations is maintained and distribution is expanded by establishing bull trout in areas identified as suitable for potential local populations. The number of existing local populations by core area are as follows: Upper Klamath Lake, 3; Sycan River, 2; and Upper Sprague River, 7. Achieving criterion 1 entails maintaining existing local populations and establishing additional potential local populations in all core areas in the recovery unit to maintain current and recovered distribution. To achieve criterion 1 and to ensure a core area population of no fewer than 100 adult bull trout, establishing at least 5 to 7 local populations in the Klamath Lake core area among 15 potential local populations (2 to 5 new local populations), at least 5 to 7 local populations in the Sycan River core area from among 15 potential local populations (3 to 5 new local populations), and at least 10 to 12 local populations in the Upper Sprague River core area from among 25 potential local populations (3 to 5 new local populations) is necessary. 2. Abundance criteria will be met when the estimated number of adult bull trout is at least 8,250 individuals distributed among the Upper Klamath Lake, Sycan River, and Upper Sprague River core areas, based on 10 years of monitoring data. 3. Trend criteria will be met when adult bull trout exhibit stable or increasing trends in abundance in the Upper Klamath Lake, Sycan River, and Upper Sprague River core areas, based on 2 generations (10 years) of monitoring data. VI 4. Connectivity criteria will be met when specific barriers to bull trout migration in the Klamath River Recovery Unit have been addressed. In the Klamath River Recovery Unit, this objective means addressing passage: 1) existing culverts that impede passage should be replaced, including those on Threemile Creek at U.S. Forest Service Road 110 crossing, Brownsworth Creek at U.S. Forest Service Road 34 crossing, and Brownsworth Creek both 0.75 mile and 1.25 miles above U.S. Forest Service Road 34; the culvert 0.25 mile below U.S. Forest Service Road 34 (to prevent repeated washout); the large-diameter culvert at the Boulder Creek road crossing; culverts in the upper Sycan River watershed that are identified in the Fremont National Forest inventory; and several in the North Fork Sprague River drainage, namely, on North Fork Sprague River (2), Boulder Creek (1), Dead Cow Creek (1), and Sheepy Creek (1); 2) fish passage structures should be installed at water diversions on bull trout streams, and barriers should be removed, including on Cherry, Sevenmile, Sun, and Threemile Creeks; 3) fish screens should be installed to prevent fish from entering diversion canals or pipes, including on Long, Deming, Threemile, Sun, Sevenmile, and Cherry Creeks; 4) manmade barriers and entrainment should be evaluated and remedied to promote migratory bull trout; priority watersheds include Threemile, Long, Deming, Sevenmile, Cherry, Sun, and Long Creeks. The Klamath River Recovery Unit team expects that the recovery process will be dynamic and will be refined as more information becomes available. Future adaptive management will play a major role in recovery implementation and refinement of recovery criteria. The recovery unit criteria listed above will be used to determine when the Klamath River Recovery Unit is fully contributing to recovery of the Klamath River population segment. vn ACTIONS NEEDED Recovery for bull trout will entail reducing threats to the long-term persistence of populations and their habitats, ensuring the security of multiple interacting groups of bull trout, and providing habitat and access to conditions that allow for the expression of various life history forms. The seven categories are listed in Chapter 1; tasks specific to this recovery unit are provided in this chapter. ESTIMATED COST OF RECOVERY Total cost of bull trout recovery in the Klamath River Recovery Unit is estimated at about $26 million spread over a 25-year recovery period. Successful recovery of bull trout in the recovery unit is contingent on removing threats from nonnative species, eliminating barriers to fish movement, and improving habitat conditions within the Klamath River basin. Total cost includes estimates of expenditures by local, Tribal, State, and Federal governments and by private business and individuals. Cost estimates are not provided for tasks which are normal agency responsibilities under existing authorities. The estimated costs are attributed to bull trout conservation, but other aquatic species will also benefit. ESTIMATED DATE OF RECOVERY Time required to achieve recovery depends on bull trout status, factors affecting bull trout, implementation and effectiveness of recovery tasks, and responses to recovery tasks. A tremendous amount of work will be required to restore impaired habitat, reconnect habitat, and eliminate threats from nonnative species. Three to five bull trout generations (15 to 25 years), or possibly longer, may be necessary before identified threats to the species can be significantly reduced and bull trout can be considered eligible for delisting. vin

1565. [Image] Geological limnology of Crater Lake, Oregon


	ill.; Three folded plates in pocket; Thesis (M.S.)--University of Minnesota, 1961; Bibliography: leaves 168-175
	Citation Citation Citation Abstract Copy Title: Geological limnology of Crater Lake, Oregon Author: Nelson, C. Hans (Carlton Hans), 1937- Year: 1961, 2008 ill.; Three folded plates in pocket; Thesis (M.S.)--University of Minnesota, 1961; Bibliography: leaves 168-175 Title: Geological limnology of Crater Lake, Oregon Author: Nelson, C. Hans (Carlton Hans), 1937- Year: 1961, 2008 ill.; Three folded plates in pocket; Thesis (M.S.)--University of Minnesota, 1961; Bibliography: leaves 168-175

1566. [Image] Geology and ground-water resources of the Swan Lake-Yonna Valleys area, Klamath County, Oregon


	Abstract The Swan Lake-Yonna Valleys area consists of two intermountain valleys with their subordinate side valleys adjoining slopes, and mountainous boundary ridges, In all the area covered is about 256 ...
	Citation Citation Citation Abstract Copy Title: Geology and ground-water resources of the Swan Lake-Yonna Valleys area, Klamath County, Oregon Author: Meyers, Joseph D. Year: 1952, 2007, 2005 Abstract The Swan Lake-Yonna Valleys area consists of two intermountain valleys with their subordinate side valleys adjoining slopes, and mountainous boundary ridges, In all the area covered is about 256 square miles but the essential agricultural sections are restricted to the floors of Swan Lake and Yonna valleys with their respective subsidiary extensions of Pine Flats and Alkali Lake flats, a valley-floor area totaling about 90 square miles The floors of Swan Lake Valley and Yonna Valley lie at an altitude of about U52OO feet but the mountainous boundary ridges rise generally to 6000 feeto Yonna Valley is largely drained to Lost River by Buck Creek but also in part to Alkali Lakeo Swan Lake Valley and Pine Flats have only internal drainage. The Swan Lake Valley floor is the top of a deep alluvial fill, while Yonna Valley floor is mainly an erosional surface sloping to lines of through drainage Precipitation is about lit inches annually on the valley floors 9 but must be much more, possibly 18 to 24 inches, on the higher parts of the drainage basins. The growing season is short and killing frosts do occur in late spring and early fall. The rock units forming the bedrock structure of the area are consolidated or semiconsolidated rocks of Tertiary age and are largely of volcanic-flow and volcanic-sedimentary originc They consist of three main elements, a lower lava-rock unit, a sedimentary and volcanic-sedimentary unit, and an upper lava-rock unito The unconsolidated deposits are the older alluvium of Quaternary (and in part of late-Tertiary) age and the younger alluvium of Quaternary age0 The bedrock is faulted and deformed particularly so along a northwest-southeast set of fault lines that have given a remarkable linearity to the topography. Unpublished records subject to revision Ground water occurs below a regional water table that slopes south-ward to the level of the Lost Rivero The upper lava rocks and the lower lava rocks contain the principal permeable zones that occur beneath the areao Breccia and other porous zones in those rocks in places yield water to wells at a rate as large as 35OOO gallons per minute with but 1 or 2 feet of drawdowno The economical construction of irrigation wells requires the determination of the best possible location at which those rocks may be tapped at shallow depth below the level of the water tableo The ground water in general relatively low in dissolved mineral matter and is but slightly to moderately hard and would be considered chemically satisfactory for most uaeso Irrigation is the principal use of the ground water in the area north of the Horsefly Irrigation Districto There 3? wells supplied about 6,000 acre-feet of water to about 3800 acres of land in 1950. Water-level records obtained since 19U8 and approximations of the probable annual recharge from precipitation indicate that the present withdrawals are considerably less than the annual increment of the ground-water recharge, Rough estimates indicate that an increase in withdrawals of as much as 100 percent or more can take place before ground-water levels, by a persistent lowering, will begin to indicate that the annual replenishment is being exceeded. Title: Geology and ground-water resources of the Swan Lake-Yonna Valleys area, Klamath County, Oregon Author: Meyers, Joseph D. Year: 1952, 2007, 2005 Abstract The Swan Lake-Yonna Valleys area consists of two intermountain valleys with their subordinate side valleys adjoining slopes, and mountainous boundary ridges, In all the area covered is about 256 square miles but the essential agricultural sections are restricted to the floors of Swan Lake and Yonna valleys with their respective subsidiary extensions of Pine Flats and Alkali Lake flats, a valley-floor area totaling about 90 square miles The floors of Swan Lake Valley and Yonna Valley lie at an altitude of about U52OO feet but the mountainous boundary ridges rise generally to 6000 feeto Yonna Valley is largely drained to Lost River by Buck Creek but also in part to Alkali Lakeo Swan Lake Valley and Pine Flats have only internal drainage. The Swan Lake Valley floor is the top of a deep alluvial fill, while Yonna Valley floor is mainly an erosional surface sloping to lines of through drainage Precipitation is about lit inches annually on the valley floors 9 but must be much more, possibly 18 to 24 inches, on the higher parts of the drainage basins. The growing season is short and killing frosts do occur in late spring and early fall. The rock units forming the bedrock structure of the area are consolidated or semiconsolidated rocks of Tertiary age and are largely of volcanic-flow and volcanic-sedimentary originc They consist of three main elements, a lower lava-rock unit, a sedimentary and volcanic-sedimentary unit, and an upper lava-rock unito The unconsolidated deposits are the older alluvium of Quaternary (and in part of late-Tertiary) age and the younger alluvium of Quaternary age0 The bedrock is faulted and deformed particularly so along a northwest-southeast set of fault lines that have given a remarkable linearity to the topography. Unpublished records subject to revision Ground water occurs below a regional water table that slopes south-ward to the level of the Lost Rivero The upper lava rocks and the lower lava rocks contain the principal permeable zones that occur beneath the areao Breccia and other porous zones in those rocks in places yield water to wells at a rate as large as 35OOO gallons per minute with but 1 or 2 feet of drawdowno The economical construction of irrigation wells requires the determination of the best possible location at which those rocks may be tapped at shallow depth below the level of the water tableo The ground water in general relatively low in dissolved mineral matter and is but slightly to moderately hard and would be considered chemically satisfactory for most uaeso Irrigation is the principal use of the ground water in the area north of the Horsefly Irrigation Districto There 3? wells supplied about 6,000 acre-feet of water to about 3800 acres of land in 1950. Water-level records obtained since 19U8 and approximations of the probable annual recharge from precipitation indicate that the present withdrawals are considerably less than the annual increment of the ground-water recharge, Rough estimates indicate that an increase in withdrawals of as much as 100 percent or more can take place before ground-water levels, by a persistent lowering, will begin to indicate that the annual replenishment is being exceeded.

1567. [Image] Scientific disagreement regarding coho salmon status under the ESA


	Internal memo between staff of the National Marine Fisheries Service dated September 27, 1996 which summarizes the issues of scientific disagreement related to the listing of three coho salmon as an endangered ...
	Citation Citation Citation Abstract Copy Title: Scientific disagreement regarding coho salmon status under the ESA Author: Varanasi, Usha; Tillman, Michael Year: 1996, 2005 Internal memo between staff of the National Marine Fisheries Service dated September 27, 1996 which summarizes the issues of scientific disagreement related to the listing of three coho salmon as an endangered species Title: Scientific disagreement regarding coho salmon status under the ESA Author: Varanasi, Usha; Tillman, Michael Year: 1996, 2005 Internal memo between staff of the National Marine Fisheries Service dated September 27, 1996 which summarizes the issues of scientific disagreement related to the listing of three coho salmon as an endangered species

1568. [Image] Improving salmon passage: draft, the Lower Snake River juvenile salmon migration feasibility report/environmental impact statement


	The purpose of this summary report is to provide an overview of the findings developed for the Lower Snake River Juvenile Salmon Migration Feasibility Study. For more detailed information, the reader should ...
	Citation Citation Citation Abstract Copy Title: Improving salmon passage: draft, the Lower Snake River juvenile salmon migration feasibility report/environmental impact statement Year: 1999, 2004 The purpose of this summary report is to provide an overview of the findings developed for the Lower Snake River Juvenile Salmon Migration Feasibility Study. For more detailed information, the reader should refer to the Draft Feasibility Report/Environmental Impact Statement and attached appendices. The genesis of this study is the National Marine Fisheries Service's 1995 Biological Opinion for the Reinitiation of Consultation on 1994-1998 Operation of the Federal Columbia River Power System and Juvenile Transportation Program in 1995 and Future Years (95 Biological Opinion). While the focus of this study is the relationship between the four dams on the lower Snake River and their effects on juvenile fish traveling toward the ocean, the implications of the study are broader. The Draft Feasibility Report/Environmental Impact Statement includes the best available information on the biological effectiveness, engineering, economic effects, and other environmental effects associated with the four specific alternatives. It does not, however, include a recommendation or identify a preferred alternative. This will give the public and other agencies an opportunity to review and understand this information and provide input before a preferred alternative is selected. At the same time, this will allow the region to consider the Habitat, Hatcheries, Harvest, and Hydropower Working Paper on salmon recovery by the Federal Caucus. Information from this process will be fully examined to determine how it may influence decisions on actions for the lower Snake River. Title: Improving salmon passage: draft, the Lower Snake River juvenile salmon migration feasibility report/environmental impact statement Year: 1999, 2004 The purpose of this summary report is to provide an overview of the findings developed for the Lower Snake River Juvenile Salmon Migration Feasibility Study. For more detailed information, the reader should refer to the Draft Feasibility Report/Environmental Impact Statement and attached appendices. The genesis of this study is the National Marine Fisheries Service's 1995 Biological Opinion for the Reinitiation of Consultation on 1994-1998 Operation of the Federal Columbia River Power System and Juvenile Transportation Program in 1995 and Future Years (95 Biological Opinion). While the focus of this study is the relationship between the four dams on the lower Snake River and their effects on juvenile fish traveling toward the ocean, the implications of the study are broader. The Draft Feasibility Report/Environmental Impact Statement includes the best available information on the biological effectiveness, engineering, economic effects, and other environmental effects associated with the four specific alternatives. It does not, however, include a recommendation or identify a preferred alternative. This will give the public and other agencies an opportunity to review and understand this information and provide input before a preferred alternative is selected. At the same time, this will allow the region to consider the Habitat, Hatcheries, Harvest, and Hydropower Working Paper on salmon recovery by the Federal Caucus. Information from this process will be fully examined to determine how it may influence decisions on actions for the lower Snake River.

1569. [Image] Volcano and earthquake hazards in the Crater Lake Region, Oregon: open file report 97-487


	ill., maps; Folded map in back cover; Includes bibliographical references ( p. 27-30) and glossary; Report accompanied by: Volcano hazard zones, volcanic vents, faults in the Crater Lake Region, Oregon ...
	Citation Citation Citation Abstract Copy Title: Volcano and earthquake hazards in the Crater Lake Region, Oregon: open file report 97-487 Author: Bacon, Charles R. Year: 1997, 2008 ill., maps; Folded map in back cover; Includes bibliographical references ( p. 27-30) and glossary; Report accompanied by: Volcano hazard zones, volcanic vents, faults in the Crater Lake Region, Oregon [map] Title: Volcano and earthquake hazards in the Crater Lake Region, Oregon: open file report 97-487 Author: Bacon, Charles R. Year: 1997, 2008 ill., maps; Folded map in back cover; Includes bibliographical references ( p. 27-30) and glossary; Report accompanied by: Volcano hazard zones, volcanic vents, faults in the Crater Lake Region, Oregon [map]

1570. [Image] The estimation of regional secondary benefits resulting from an improvement in water quality of Upper Klamath Lake, Oregon: an interindustry approach


	AN ABSTRACT OF THE THESIS OF STEPHEN DOUGLAS REILING for the MASTER OF SCIENCE (Name) (Degree) in AGRICULTURAL ECONOMICS presented on (Major) (Date) Title: THE ESTIMATION OF REGIONAL ...
	Citation Citation Citation Abstract Copy Title: The estimation of regional secondary benefits resulting from an improvement in water quality of Upper Klamath Lake, Oregon: an interindustry approach Author: Reiling, Stephen Douglas Year: 1971, 2006, 2005 AN ABSTRACT OF THE THESIS OF STEPHEN DOUGLAS REILING for the MASTER OF SCIENCE (Name) (Degree) in AGRICULTURAL ECONOMICS presented on (Major) (Date) Title: THE ESTIMATION OF REGIONAL SECONDARY BENEFITS RESULTING FROM AN IMPROVEMENT IN WATER QUALITY OF UPPER KLAMATH LAKE, OREGON; AN INTERINDUSTRY APPROACH Abstract approved^ Herbert H. Stoevener The primary objective of this study was to estimate the impact that an increase in recreational expenditures, resulting from water quality improvements of Klamath Lake, would have upon the Klamath County economy. As the sales of the economy expand to serve the needs of the recreationists, real benefits will be forthcoming to the businesses and households of the county in the forms of more business and higher incomes., To estimate the total impact of the increased volume of recreational expenditures that may be made in the economy, the economic relationships of the local economy h Title: The estimation of regional secondary benefits resulting from an improvement in water quality of Upper Klamath Lake, Oregon: an interindustry approach Author: Reiling, Stephen Douglas Year: 1971, 2006, 2005 AN ABSTRACT OF THE THESIS OF STEPHEN DOUGLAS REILING for the MASTER OF SCIENCE (Name) (Degree) in AGRICULTURAL ECONOMICS presented on (Major) (Date) Title: THE ESTIMATION OF REGIONAL SECONDARY BENEFITS RESULTING FROM AN IMPROVEMENT IN WATER QUALITY OF UPPER KLAMATH LAKE, OREGON; AN INTERINDUSTRY APPROACH Abstract approved^ Herbert H. Stoevener The primary objective of this study was to estimate the impact that an increase in recreational expenditures, resulting from water quality improvements of Klamath Lake, would have upon the Klamath County economy. As the sales of the economy expand to serve the needs of the recreationists, real benefits will be forthcoming to the businesses and households of the county in the forms of more business and higher incomes., To estimate the total impact of the increased volume of recreational expenditures that may be made in the economy, the economic relationships of the local economy h

1571. [Image] Bull Trout, Salvelinus Confluentus... Draft Recovery Plan, Chapter 1, Introduction...


	EXECUTIVE SUMMARY FOR THE BULL TROUT RECOVERY PLAN Current Species Status The bull trout (Salvelinus confluentus) in the coterminous United States was listed as threatened on November 1, 1999 (64 ...
	Citation Citation Citation Abstract Copy Title: Bull Trout, Salvelinus Confluentus... Draft Recovery Plan, Chapter 1, Introduction... Author: U.S. Fish and Wildlife Service Year: 2003, 2008, 2005 EXECUTIVE SUMMARY FOR THE BULL TROUT RECOVERY PLAN Current Species Status The bull trout (Salvelinus confluentus) in the coterminous United States was listed as threatened on November 1, 1999 (64 FR 58910). Earlier rulemakings had listed distinct population segments of bull trout as threatened in the Columbia River, Klamath River, and Jarbidge River basins (63 FR 31647, 63 FR 42757, 64 FR 17110). Bull trout distribution, abundance, and habitat quality have declined rangewide. Several local extirpations have been documented, beginning in the 1950fs. Bull trout continue to occur the Klamath River, Columbia River, Jarbidge River, St. Mary-Belly River, and Coastal-Puget Sound, in the states of Idaho, Montana, Nevada, Oregon, and Washington. Habitat Requirements and Limiting Factors Bull trout have more specific habitat requirements than most other salmonids. Habitat components that influence bull trout distribution and abundance include water temperature, cover, channel form and stability, substrate for spawning and rearing, and migratory corridors. Bull trout are found in colder streams and require colder water than most other salmonids for incubation, juvenile rearing, and spawning. Spawning and rearing areas are often associated with cold-water springs, groundwater infiltration, and/or the coldest streams in a watershed. Throughout their lives, bull trout require complex forms of cover, including large woody debris, undercut banks, boulders, and pools. Alterations in channel form and reductions in channel stability result in habitat degradation and reduced survival of bull trout eggs and juveniles. Channel alterations may reduce the abundance and quality of side channels, stream margins, and pools, which are areas bull trout frequently inhabit. For spawning and early rearing bull trout require loose, clean gravel relatively free of fine sediments. Because bull trout have a relatively long incubation and development period within spawning gravel (greater than 200 days), transport of bedload in unstable channels may kill young bull trout. Bull trout use migratory corridors to move from spawning and rearing habitats to foraging and overwintering habitats and back. Different habitats provide bull trout with diverse resources, and migratory corridors allow local populations to connect, which may increase the potential for gene flow and support or refounding of populations. Declines in bull trout distribution and abundance are the results of combined effects of the following: habitat degradation and fragmentation, the blockage of migratory corridors, poor water quality, angler harvest and poaching, entrainment (process by which aquatic organisms are pulled through a diversion structure or other device) into diversion channels and dams, and introduced iv normative species. Specific land and water management activities that continue to depress bull trout populations and degrade habitat include dams and other diversion structures, forest management practices, livestock grazing, agriculture, road construction and maintenance, mining, and urban and rural development. Some threats to bull trout are the continuing effects of past land management activities. Organization and Development of the Recovery Plan Because bull trout in the coterminous United States are widely distributed within a large area, the recovery plan is organized into multiple chapters. This introductory chapter (Chapter 1) describes our overall recovery strategy for the species, defines recovery, and identifies recovery actions applicable for all listed bull trout in the coterminous United States. Each successive chapter focuses on bull trout in specific geographic areas (recovery units), and describes conditions, defines recovery criteria, and identifies specific recovery actions for the recovery unit. Recovery Objectives The goal of this recovery plan is to describe the actions needed to achieve the recovery of bull trout, that is, to ensure the long-term persistence of self-sustaining, complex interacting groups (or multiple local populations that may have overlapping spawning and rearing areas) of bull trout distributed across the species' native range. Recovery of bull trout will require reducing threats to the long-term persistence of populations, maintaining multiple interconnected populations of bull trout across the diverse habitats of their native range, and preserving the diversity of bull trout life-history strategies (e.g., resident or migratory forms, emigration age, spawning frequency, local habitat adaptations). To recover bull trout, the following four objectives have been identified: ? Maintain current distribution of bull trout within core areas as described in recovery unit chapters and restore distribution where recommended in recovery unit chapters. ? Maintain stable or increasing trend in abundance of bull trout. ? Restore and maintain suitable habitat conditions for all bull trout life history stages and strategies. ? Conserve genetic diversity and provide opportunity for genetic exchange. ? These objectives apply to bull trout in all recovery units. Additional objectives may be necessary to achieve recovery in some recovery units and will be identified in the respective recovery unit chapters. Recovery Criteria Criteria are established to assess whether recovery objectives are being achieved. Criteria specific to each recovery unit are defined in each recovery unit chapter. Individual chapters may contain criteria for assessing the status of bull trout and alleviation of threats that are unique to one or several recovery units. However, every recovery unit chapter will contain criteria that address the following characteristics: ? The distribution of bull trout in identified and potential local populations in all core areas within the recovery unit. ? The estimated abundance of adult bull trout within core areas in the recovery unit, expressed as either a point estimate or a range of individuals. ? The presence of stable or increasing trends for adult bull trout abundance in the recovery unit. ? The restoration of passage at specific barriers identified as inhibiting recovery. We expect recovery of bull trout to be a dynamic process occurring over time. The recovery objectives are based on our current knowledge and may be refined as more information becomes available. Some local populations of bull trout, and possibly core area populations, may be extirpated even though recovery actions are being implemented. If reestablishment of recently extirpated populations is not feasible or practical, recovery criteria for a given recovery unit will be revised on a case-by-case basis. Meeting the four recovery criteria is not intended to be precluded where localized extirpations of bull trout are offset by sufficiently strong improvements in other areas of a recovery unit in meeting the four recovery objectives. The determination of whether a distinct population segment of bull trout is recovered will rely on an analysis of the overall status of the species, threats to the species, and the adequacy of existing regulatory and conservation mechanisms. For example, it may be possible for the Columbia River Distinct Population Segment, which has 22 recovery units, to be recovered prior to all recovery unit criteria being met in all recovery units. Success in accomplishing the recovery VI criteria will be reviewed and considered for the impacts both within a recovery unit and throughout a distinct population segment. Actions Needed Specific tasks falling within the following seven categories will be necessary to initiate recovery within all recovery units: ? Protect, restore, and maintain suitable habitat conditions for bull trout. ? Prevent and reduce negative effects of normative fishes and other normative taxa on bull trout. ? Establish fisheries management goals and objectives compatible with bull trout recovery and implement practices to achieve goals. ? Characterize, conserve, and monitor genetic diversity and gene flow among local populations of bull trout. ? Conduct research and monitoring to implement and evaluate bull trout recovery activities, consistent with an adaptive management approach using feedback from implemented, site-specific recovery tasks. ? Use all available conservation programs and regulations to protect and conserve bull trout and bull trout habitats. ? Assess the implementation of bull trout recovery by recovery units and revise recovery unit plans based on evaluations. Recovery Priority Number The recovery priority number for bull trout in the coterminous United States is 9C, on a scale of 1 to 18, indicating that (1) taxonomically, these populations are distinct population segments of a species, (2) the five populations are subject to a moderate degree of threat(s), (3) the recovery potential is high, and (4) the degree of potential conflict during recovery is high. vrr Estimated Cost of Recovery The total cost estimate of recovery for bull trout in the coterminous United States is presented in the individual recovery unit chapters. The costs presented in each chapter are attributed to bull trout conservation but other species will also benefit. Date of Recovery Expected time to achieve recovery varies among recovery units because of differences in bull trout status, factors affecting bull trout, implementation and effectiveness of recovery tasks, and responses to recovery tasks. Achieving bull trout recovery in all recovery units will be a complex process that will likely take 25 years or more. vin Title: Bull Trout, Salvelinus Confluentus... Draft Recovery Plan, Chapter 1, Introduction... Author: U.S. Fish and Wildlife Service Year: 2003, 2008, 2005 EXECUTIVE SUMMARY FOR THE BULL TROUT RECOVERY PLAN Current Species Status The bull trout (Salvelinus confluentus) in the coterminous United States was listed as threatened on November 1, 1999 (64 FR 58910). Earlier rulemakings had listed distinct population segments of bull trout as threatened in the Columbia River, Klamath River, and Jarbidge River basins (63 FR 31647, 63 FR 42757, 64 FR 17110). Bull trout distribution, abundance, and habitat quality have declined rangewide. Several local extirpations have been documented, beginning in the 1950fs. Bull trout continue to occur the Klamath River, Columbia River, Jarbidge River, St. Mary-Belly River, and Coastal-Puget Sound, in the states of Idaho, Montana, Nevada, Oregon, and Washington. Habitat Requirements and Limiting Factors Bull trout have more specific habitat requirements than most other salmonids. Habitat components that influence bull trout distribution and abundance include water temperature, cover, channel form and stability, substrate for spawning and rearing, and migratory corridors. Bull trout are found in colder streams and require colder water than most other salmonids for incubation, juvenile rearing, and spawning. Spawning and rearing areas are often associated with cold-water springs, groundwater infiltration, and/or the coldest streams in a watershed. Throughout their lives, bull trout require complex forms of cover, including large woody debris, undercut banks, boulders, and pools. Alterations in channel form and reductions in channel stability result in habitat degradation and reduced survival of bull trout eggs and juveniles. Channel alterations may reduce the abundance and quality of side channels, stream margins, and pools, which are areas bull trout frequently inhabit. For spawning and early rearing bull trout require loose, clean gravel relatively free of fine sediments. Because bull trout have a relatively long incubation and development period within spawning gravel (greater than 200 days), transport of bedload in unstable channels may kill young bull trout. Bull trout use migratory corridors to move from spawning and rearing habitats to foraging and overwintering habitats and back. Different habitats provide bull trout with diverse resources, and migratory corridors allow local populations to connect, which may increase the potential for gene flow and support or refounding of populations. Declines in bull trout distribution and abundance are the results of combined effects of the following: habitat degradation and fragmentation, the blockage of migratory corridors, poor water quality, angler harvest and poaching, entrainment (process by which aquatic organisms are pulled through a diversion structure or other device) into diversion channels and dams, and introduced iv normative species. Specific land and water management activities that continue to depress bull trout populations and degrade habitat include dams and other diversion structures, forest management practices, livestock grazing, agriculture, road construction and maintenance, mining, and urban and rural development. Some threats to bull trout are the continuing effects of past land management activities. Organization and Development of the Recovery Plan Because bull trout in the coterminous United States are widely distributed within a large area, the recovery plan is organized into multiple chapters. This introductory chapter (Chapter 1) describes our overall recovery strategy for the species, defines recovery, and identifies recovery actions applicable for all listed bull trout in the coterminous United States. Each successive chapter focuses on bull trout in specific geographic areas (recovery units), and describes conditions, defines recovery criteria, and identifies specific recovery actions for the recovery unit. Recovery Objectives The goal of this recovery plan is to describe the actions needed to achieve the recovery of bull trout, that is, to ensure the long-term persistence of self-sustaining, complex interacting groups (or multiple local populations that may have overlapping spawning and rearing areas) of bull trout distributed across the species' native range. Recovery of bull trout will require reducing threats to the long-term persistence of populations, maintaining multiple interconnected populations of bull trout across the diverse habitats of their native range, and preserving the diversity of bull trout life-history strategies (e.g., resident or migratory forms, emigration age, spawning frequency, local habitat adaptations). To recover bull trout, the following four objectives have been identified: ? Maintain current distribution of bull trout within core areas as described in recovery unit chapters and restore distribution where recommended in recovery unit chapters. ? Maintain stable or increasing trend in abundance of bull trout. ? Restore and maintain suitable habitat conditions for all bull trout life history stages and strategies. ? Conserve genetic diversity and provide opportunity for genetic exchange. ? These objectives apply to bull trout in all recovery units. Additional objectives may be necessary to achieve recovery in some recovery units and will be identified in the respective recovery unit chapters. Recovery Criteria Criteria are established to assess whether recovery objectives are being achieved. Criteria specific to each recovery unit are defined in each recovery unit chapter. Individual chapters may contain criteria for assessing the status of bull trout and alleviation of threats that are unique to one or several recovery units. However, every recovery unit chapter will contain criteria that address the following characteristics: ? The distribution of bull trout in identified and potential local populations in all core areas within the recovery unit. ? The estimated abundance of adult bull trout within core areas in the recovery unit, expressed as either a point estimate or a range of individuals. ? The presence of stable or increasing trends for adult bull trout abundance in the recovery unit. ? The restoration of passage at specific barriers identified as inhibiting recovery. We expect recovery of bull trout to be a dynamic process occurring over time. The recovery objectives are based on our current knowledge and may be refined as more information becomes available. Some local populations of bull trout, and possibly core area populations, may be extirpated even though recovery actions are being implemented. If reestablishment of recently extirpated populations is not feasible or practical, recovery criteria for a given recovery unit will be revised on a case-by-case basis. Meeting the four recovery criteria is not intended to be precluded where localized extirpations of bull trout are offset by sufficiently strong improvements in other areas of a recovery unit in meeting the four recovery objectives. The determination of whether a distinct population segment of bull trout is recovered will rely on an analysis of the overall status of the species, threats to the species, and the adequacy of existing regulatory and conservation mechanisms. For example, it may be possible for the Columbia River Distinct Population Segment, which has 22 recovery units, to be recovered prior to all recovery unit criteria being met in all recovery units. Success in accomplishing the recovery VI criteria will be reviewed and considered for the impacts both within a recovery unit and throughout a distinct population segment. Actions Needed Specific tasks falling within the following seven categories will be necessary to initiate recovery within all recovery units: ? Protect, restore, and maintain suitable habitat conditions for bull trout. ? Prevent and reduce negative effects of normative fishes and other normative taxa on bull trout. ? Establish fisheries management goals and objectives compatible with bull trout recovery and implement practices to achieve goals. ? Characterize, conserve, and monitor genetic diversity and gene flow among local populations of bull trout. ? Conduct research and monitoring to implement and evaluate bull trout recovery activities, consistent with an adaptive management approach using feedback from implemented, site-specific recovery tasks. ? Use all available conservation programs and regulations to protect and conserve bull trout and bull trout habitats. ? Assess the implementation of bull trout recovery by recovery units and revise recovery unit plans based on evaluations. Recovery Priority Number The recovery priority number for bull trout in the coterminous United States is 9C, on a scale of 1 to 18, indicating that (1) taxonomically, these populations are distinct population segments of a species, (2) the five populations are subject to a moderate degree of threat(s), (3) the recovery potential is high, and (4) the degree of potential conflict during recovery is high. vrr Estimated Cost of Recovery The total cost estimate of recovery for bull trout in the coterminous United States is presented in the individual recovery unit chapters. The costs presented in each chapter are attributed to bull trout conservation but other species will also benefit. Date of Recovery Expected time to achieve recovery varies among recovery units because of differences in bull trout status, factors affecting bull trout, implementation and effectiveness of recovery tasks, and responses to recovery tasks. Achieving bull trout recovery in all recovery units will be a complex process that will likely take 25 years or more. vin

1572. [Image] Past, present and future activities being conducted in the Klamath River Basin related to the protection and recovery of fish and their habitat


	"March 2003"
	Citation Citation Citation Abstract Copy Title: Past, present and future activities being conducted in the Klamath River Basin related to the protection and recovery of fish and their habitat Author: United States. National Marine Fisheries Service Year: 2003, 2005 "March 2003" Title: Past, present and future activities being conducted in the Klamath River Basin related to the protection and recovery of fish and their habitat Author: United States. National Marine Fisheries Service Year: 2003, 2005 "March 2003"

1573. [Image] The doctrine of prior appropriation : effects upon water rights in the Upper Klamath Basin


	Undergraduate student project, Geomatics 466, Boundary Law II
	Citation Citation Citation Abstract Copy Title: The doctrine of prior appropriation : effects upon water rights in the Upper Klamath Basin Author: Hellebust, Kane Year: 2004, 2005 Undergraduate student project, Geomatics 466, Boundary Law II Title: The doctrine of prior appropriation : effects upon water rights in the Upper Klamath Basin Author: Hellebust, Kane Year: 2004, 2005 Undergraduate student project, Geomatics 466, Boundary Law II

1574. [Image] Data from pumping and injection tests and chemical sampling in the geothermal aquifer at Klamath Falls,


	DATA FROM PUMPING AND INJECTION TESTS AND CHEMICAL SAMPLING IN THE GEOTHERMAL AQUIFER AT KLAMATH FALLS, OREGON By S. M. Benson? , C. J. Janik ? , D. C. Longi , R. D. ...
	Citation Citation Citation Abstract Copy Title: Data from pumping and injection tests and chemical sampling in the geothermal aquifer at Klamath Falls, Author: Benson, S. M Year: 1984, 2007, 2005 DATA FROM PUMPING AND INJECTION TESTS AND CHEMICAL SAMPLING IN THE GEOTHERMAL AQUIFER AT KLAMATH FALLS, OREGON By S. M. Benson? , C. J. Janik ? , D. C. Longi , R. D. Solbaui- , P. J. Lienau^, G. G. Culver^, E. A. Sanmel-^, S. R. Swanson^, D. M. Hart-5/, Andrew Yeei/, A. F. White!', M. L. Stallard^, A. P. Brown^, M. C. Wheeler?', T. L. Winnett? , Grace Fong?', and G. B. ^' ABSTRACT A seven-week pumping and injection test in the geothermal aquifer at Klamath Falls, Oregon, in 1983 provided new information on hydraulic properties of the aquifer* The Open-File Data Report on the tests includes graphs of water levels measured in 50 wells, temperature measurement In 17 wells, daily air-temperatures in relation to discharge of thermal water from more than 70 pumped and artesian wells, tables of monthly mean air temperatures and estimates of discharges of thermal water during a normal year, and tables of chemical and isotopic analyses on samples from 12 wells. The water-level measurements reflect the effects of pumping, injection, and recovery over about 17 square miles of the hot-well area of Klamath Falls. The pumped well, City Well #1, and the injection well at the Klamath County Museum are components of a proposed District Heating Plan. The study was funded principally under contracts from the U.S. Department of Energy to the Lawrence Berkeley Laboratory, Stanford University, and the Oregon Institute of Technology, with coordination and chemical sampling provided under the Geothermal Research Program, U.S. Geological Survey. Support was received from the City of Klamath Falls, Klamath County Chamber of Commerce, Citizens for Responsible Geothermal Development, and many citizen volunteers. ? Lawrence Berkeley Laboratory, Berkeley, California 2/ ? U.S. Geological Survey, Menlo Park, California ? Energyman, Inc., Klamath Falls, Oregon 4/ ? Oregon Institute of Technology, Klamath Falls, Oregon ? Citizens for Responsible Geothermal Development, Klamath Falls, Oregon Title: Data from pumping and injection tests and chemical sampling in the geothermal aquifer at Klamath Falls, Author: Benson, S. M Year: 1984, 2007, 2005 DATA FROM PUMPING AND INJECTION TESTS AND CHEMICAL SAMPLING IN THE GEOTHERMAL AQUIFER AT KLAMATH FALLS, OREGON By S. M. Benson? , C. J. Janik ? , D. C. Longi , R. D. Solbaui- , P. J. Lienau^, G. G. Culver^, E. A. Sanmel-^, S. R. Swanson^, D. M. Hart-5/, Andrew Yeei/, A. F. White!', M. L. Stallard^, A. P. Brown^, M. C. Wheeler?', T. L. Winnett? , Grace Fong?', and G. B. ^' ABSTRACT A seven-week pumping and injection test in the geothermal aquifer at Klamath Falls, Oregon, in 1983 provided new information on hydraulic properties of the aquifer The Open-File Data Report on the tests includes graphs of water levels measured in 50 wells, temperature measurement In 17 wells, daily air-temperatures in relation to discharge of thermal water from more than 70 pumped and artesian wells, tables of monthly mean air temperatures and estimates of discharges of thermal water during a normal year, and tables of chemical and isotopic analyses on samples from 12 wells. The water-level measurements reflect the effects of pumping, injection, and recovery over about 1*7 square miles of the hot-well area of Klamath Falls. The pumped well, City Well #1, and the injection well at the Klamath County Museum are components of a proposed District Heating Plan. The study was funded principally under contracts from the U.S. Department of Energy to the Lawrence Berkeley Laboratory, Stanford University, and the Oregon Institute of Technology, with coordination and chemical sampling provided under the Geothermal Research Program, U.S. Geological Survey. Support was received from the City of Klamath Falls, Klamath County Chamber of Commerce, Citizens for Responsible Geothermal Development, and many citizen volunteers. ? Lawrence Berkeley Laboratory, Berkeley, California 2/ ? U.S. Geological Survey, Menlo Park, California ? Energyman, Inc., Klamath Falls, Oregon 4/ ? Oregon Institute of Technology, Klamath Falls, Oregon ? Citizens for Responsible Geothermal Development, Klamath Falls, Oregon

1575. [Image] The geology and petrography of Crater Lake National Park


	maps; Geology by J.S. Diller. Petrography by H.B. Patton
	Citation Citation Citation Abstract Copy Title: The geology and petrography of Crater Lake National Park Author: Diller, J. S. (Joseph Silas), b. 1850; Patton, Horace Bushnell, 1858-1929 Year: 1902, 2008 maps; Geology by J.S. Diller. Petrography by H.B. Patton Title: The geology and petrography of Crater Lake National Park Author: Diller, J. S. (Joseph Silas), b. 1850; Patton, Horace Bushnell, 1858-1929 Year: 1902, 2008 maps; Geology by J.S. Diller. Petrography by H.B. Patton

1576. [Image] Dear concerned citizen


	"Bureau of Land Management's (BLM) proposed decision and finding of no significant impact for the Lost River Management Framework Plan amendments."-- P. [1]; August 19, 1988."; "BLM-OR-PT-88-12-1792"--P. ...
	Citation Citation Citation Abstract Copy Title: Dear concerned citizen Year: 1988, 2005 "Bureau of Land Management's (BLM) proposed decision and finding of no significant impact for the Lost River Management Framework Plan amendments."-- P. [1]; August 19, 1988."; "BLM-OR-PT-88-12-1792"--P. 8 Title: Dear concerned citizen Year: 1988, 2005 "Bureau of Land Management's (BLM) proposed decision and finding of no significant impact for the Lost River Management Framework Plan amendments."-- P. [1]; August 19, 1988."; "BLM-OR-PT-88-12-1792"--P. 8

1577. [Image] Nutrient loading of surface waters in the Upper Klamath Basin : agricultural and natural sources


	Abstract Implementation of the Federal Clean Water Act and Oregon Senate Bill 1010 is proceeding under two simultaneous processes in Oregon. The Oregon Department of Environmental Quality is responsible ...
	Citation Citation Citation Abstract Copy Title: Nutrient loading of surface waters in the Upper Klamath Basin : agricultural and natural sources Author: Rykbost, K. A. Year: 2001, 2004 Abstract Implementation of the Federal Clean Water Act and Oregon Senate Bill 1010 is proceeding under two simultaneous processes in Oregon. The Oregon Department of Environmental Quality is responsible for developing Total Maximum Daily Load (TMDL) allocations for water-quality limited water bodies. The Oregon Department of Agriculture is striving to develop Management Area Plans to provide guidance for management of private agricultural lands to meet Clean Water Act objectives. Both processes seek input from local advisory committees comprised of landowners and other stakeholders, and technical review committees. Klamath Lake and Klamath River have been designated water quality impaired for several parameters including nutrients. Researchers have attempted to determine the extent of agriculture's contributions to nutrient enrichment of surface waters in the Upper Klamath Basin. Two United States Geological Survey (USGS) studies focused attention on drainage of agricultural lands adjacent to Klamath Lake as a significant source of nutrient loading in the lake. A preliminary draft report by the Klamath River TMDL committee identified the outlet for drainage waters from the Klamath Irrigation Project to the Klamath River at the Straits Drain as a point source for nutrient loading. Preparation of a final TMDL for this sub-watershed was tabled pending development of a TMDL for Klamath Lake and its tributaries. Insufficient data are available to determine the relative contributions of agricultural activities, natural background sources, and other potential sources of nutrient enrichment to establish numerical limits for nutrient loading from agricultural lands. From 1998 through 2000, the Klamath Experiment Station has investigated nutrient loading from drainage of agricultural lands adjacent to Klamath Lake, natural background sources including major springs and several artesian wells, and loading to the Klamath Irrigation Project from diversions out of Klamath Lake and Klamath River. Findings indicate contributions from agricultural lands adjacent to Klamath Lake have been overestimated, and the Klamath Irrigation Project is probably a net sink for nutrients diverted out of Klamath Lake and Klamath River. Data to support these assertions are presented. Introduction Most of the surface waters in the Klamath Basin are included in the Oregon department of Environmental Quality (DEQ) 303D list as water-quality limited. While the only criterion for listing of many streams is temperature, based on a preliminary standard of 64°F, Klamath Lake and Klamath River are listed for chlorophyll a, dissolved oxygen, un-ionized ammonia, and pH. The DEQ is working toward development of TMDL allocations for Klamath River and Title: Nutrient loading of surface waters in the Upper Klamath Basin : agricultural and natural sources Author: Rykbost, K. A. Year: 2001, 2004 Abstract Implementation of the Federal Clean Water Act and Oregon Senate Bill 1010 is proceeding under two simultaneous processes in Oregon. The Oregon Department of Environmental Quality is responsible for developing Total Maximum Daily Load (TMDL) allocations for water-quality limited water bodies. The Oregon Department of Agriculture is striving to develop Management Area Plans to provide guidance for management of private agricultural lands to meet Clean Water Act objectives. Both processes seek input from local advisory committees comprised of landowners and other stakeholders, and technical review committees. Klamath Lake and Klamath River have been designated water quality impaired for several parameters including nutrients. Researchers have attempted to determine the extent of agriculture's contributions to nutrient enrichment of surface waters in the Upper Klamath Basin. Two United States Geological Survey (USGS) studies focused attention on drainage of agricultural lands adjacent to Klamath Lake as a significant source of nutrient loading in the lake. A preliminary draft report by the Klamath River TMDL committee identified the outlet for drainage waters from the Klamath Irrigation Project to the Klamath River at the Straits Drain as a point source for nutrient loading. Preparation of a final TMDL for this sub-watershed was tabled pending development of a TMDL for Klamath Lake and its tributaries. Insufficient data are available to determine the relative contributions of agricultural activities, natural background sources, and other potential sources of nutrient enrichment to establish numerical limits for nutrient loading from agricultural lands. From 1998 through 2000, the Klamath Experiment Station has investigated nutrient loading from drainage of agricultural lands adjacent to Klamath Lake, natural background sources including major springs and several artesian wells, and loading to the Klamath Irrigation Project from diversions out of Klamath Lake and Klamath River. Findings indicate contributions from agricultural lands adjacent to Klamath Lake have been overestimated, and the Klamath Irrigation Project is probably a net sink for nutrients diverted out of Klamath Lake and Klamath River. Data to support these assertions are presented. Introduction Most of the surface waters in the Klamath Basin are included in the Oregon department of Environmental Quality (DEQ) 303D list as water-quality limited. While the only criterion for listing of many streams is temperature, based on a preliminary standard of 64°F, Klamath Lake and Klamath River are listed for chlorophyll a, dissolved oxygen, un-ionized ammonia, and pH. The DEQ is working toward development of TMDL allocations for Klamath River and

1578. [Image] Recreational use and carrying capacity for the Klamath River


	ABSTRACT These reports document recreation use and estimate carrying capacities for the Klamath River in northern California. The river section studied runs from Interstate 5 near Yreka to the town of ...
	Citation Citation Citation Abstract Copy Title: Recreational use and carrying capacity for the Klamath River Author: Shelby, Bo Year: 1984, 2005 ABSTRACT These reports document recreation use and estimate carrying capacities for the Klamath River in northern California. The river section studied runs from Interstate 5 near Yreka to the town of Orleans, and includes the lower sections of the Scott and Salmon River tributaries. A major highway runs along the river throughout the study area, with numerous; access points. The study covers the summer river running season and the fall salmon/ steel head fishing season. Because of the differences in time periods and activities, the study was done in two separate parts, each with a separate report. This document combines the two. The summer season report is presented first, followed by the fall season report. Each of these is preceeded by its own table of contents, list of tables, and summary of findings, and each is followed by its own appendices. The reports are separated by a colored page for easy reference. Data were collected by sampling, observation, and counting as well as a user questionnaire. Th? study presents a detailed description of river sections and documents recreational use by location and activity type. Carrying capacities are estimated for both river running and fishing activities. Estimates include discussions of ecological, facility, physical, and social carrying capacities, distinguishing descriptive and evaluative components. Limiting factors vary, depending on the activity and location. The more developed setting and the variety of activities and capacities distinguishes this project from earlier river capacity studies. Title: Recreational use and carrying capacity for the Klamath River Author: Shelby, Bo Year: 1984, 2005 ABSTRACT These reports document recreation use and estimate carrying capacities for the Klamath River in northern California. The river section studied runs from Interstate 5 near Yreka to the town of Orleans, and includes the lower sections of the Scott and Salmon River tributaries. A major highway runs along the river throughout the study area, with numerous; access points. The study covers the summer river running season and the fall salmon/ steel head fishing season. Because of the differences in time periods and activities, the study was done in two separate parts, each with a separate report. This document combines the two. The summer season report is presented first, followed by the fall season report. Each of these is preceeded by its own table of contents, list of tables, and summary of findings, and each is followed by its own appendices. The reports are separated by a colored page for easy reference. Data were collected by sampling, observation, and counting as well as a user questionnaire. Th? study presents a detailed description of river sections and documents recreational use by location and activity type. Carrying capacities are estimated for both river running and fishing activities. Estimates include discussions of ecological, facility, physical, and social carrying capacities, distinguishing descriptive and evaluative components. Limiting factors vary, depending on the activity and location. The more developed setting and the variety of activities and capacities distinguishes this project from earlier river capacity studies.

1579. [Image] Weather based technologies for residential irrigation scheduling: technical review report: prepared for Municipal Water District


	"May 2004"
	Citation Citation Citation Abstract Copy Title: Weather based technologies for residential irrigation scheduling: technical review report: prepared for Municipal Water District Year: 2004, 2005 "May 2004" Title: Weather based technologies for residential irrigation scheduling: technical review report: prepared for Municipal Water District Year: 2004, 2005 "May 2004"

1580. [Image] Federal Register - Endangered and Threatened Wildlife and Plants; Definition of "Harm"


	This final rule defines the term "harm", which is contained in the definition of "take" in the Endangered Species Act (ESA). The purpose of this rulemaking is to clarify the type of actions that may result ...
	Citation Citation Citation Abstract Copy Title: Federal Register - Endangered and Threatened Wildlife and Plants; Definition of "Harm" Year: 1999, 2008, 2005 This final rule defines the term "harm", which is contained in the definition of "take" in the Endangered Species Act (ESA). The purpose of this rulemaking is to clarify the type of actions that may result in a take of a listed species under the ESA. This final rule is not a change in existing law. It provides clear notification to the public that habitat modification or degradation may harm listed species and, therefore, constitutes a take under the ESA as well as ensuring consistency between NMFS and the Fish and Wildlife Service (FWS). This final rule defines the term "harm" to include any act which actually kills or injures fish or wildlife, and emphasizes that such acts may include significant habitat modification or degradation that significantly impairs essential behavioral patterns of fish or wildlife Title: Federal Register - Endangered and Threatened Wildlife and Plants; Definition of "Harm" Year: 1999, 2008, 2005 This final rule defines the term "harm", which is contained in the definition of "take" in the Endangered Species Act (ESA). The purpose of this rulemaking is to clarify the type of actions that may result in a take of a listed species under the ESA. This final rule is not a change in existing law. It provides clear notification to the public that habitat modification or degradation may harm listed species and, therefore, constitutes a take under the ESA as well as ensuring consistency between NMFS and the Fish and Wildlife Service (FWS). This final rule defines the term "harm" to include any act which actually kills or injures fish or wildlife, and emphasizes that such acts may include significant habitat modification or degradation that significantly impairs essential behavioral patterns of fish or wildlife

1581. [Image] Forestry program for Oregon


	This document sets forth the Board of Forestry's strategic vision for Oregon's forests for the next eight years
	Citation Citation Citation Abstract Copy Title: Forestry program for Oregon Author: Oregon State Board of Forestry Year: 2003, 2005 This document sets forth the Board of Forestry's strategic vision for Oregon's forests for the next eight years Title: Forestry program for Oregon Author: Oregon State Board of Forestry Year: 2003, 2005 This document sets forth the Board of Forestry's strategic vision for Oregon's forests for the next eight years

1582. [Image] Historic resource study: Crater Lake National Park, Oregon


	ill.; "June 1984."; Bibliography: p. 307-317
	Citation Citation Citation Abstract Copy Title: Historic resource study: Crater Lake National Park, Oregon Author: Greene, Linda W. Year: 1984, 2009, 2010 ill.; "June 1984."; Bibliography: p. 307-317 Title: Historic resource study: Crater Lake National Park, Oregon Author: Greene, Linda W. Year: 1984, 2009, 2010 ill.; "June 1984."; Bibliography: p. 307-317

1583. [Image] Research information needs on terrestrial vertebrate species of the interior Columbia River basin and northern portions of the Klamath and Great basins: research, development, and application database


	"September 1997"; Includes bibliographical references (p. 24)
	Citation Citation Citation Abstract Copy Title: Research information needs on terrestrial vertebrate species of the interior Columbia River basin and northern portions of the Klamath and Great basins: research, development, and application database Author: Marcot, Bruce G. Year: 1997, 2005, 2004 "September 1997"; Includes bibliographical references (p. 24) Title: Research information needs on terrestrial vertebrate species of the interior Columbia River basin and northern portions of the Klamath and Great basins: research, development, and application database Author: Marcot, Bruce G. Year: 1997, 2005, 2004 "September 1997"; Includes bibliographical references (p. 24)

1584. [Image] National irrigation as a social problem


	Includes two scenic photos "The great gates on the Minidoka Project through which Snake River is now passing" and "From Smiley Heights, Redlands - the result of irrigation" ; The author of this article ...
	Citation Citation Citation Abstract Copy Title: National irrigation as a social problem Author: Newlands, Francis G. Year: 1906, 2005, 2004 Includes two scenic photos "The great gates on the Minidoka Project through which Snake River is now passing" and "From Smiley Heights, Redlands - the result of irrigation" ; The author of this article was the Senator of Nevada. Title: National irrigation as a social problem Author: Newlands, Francis G. Year: 1906, 2005, 2004 Includes two scenic photos "The great gates on the Minidoka Project through which Snake River is now passing" and "From Smiley Heights, Redlands - the result of irrigation" ; The author of this article was the Senator of Nevada.

1585. [Image] Annual project history: Klamath Project, Oregon-California, 1962


	Ill., maps (some color), photographs; Includes fiscal year financials, maps, photographs, agricultural economics and crop yield, some grazing financial information with cost of water usage, tables for ...
	Citation Citation Citation Abstract Copy Title: Annual project history: Klamath Project, Oregon-California, 1962 Author: United States. Bureau of Reclamation Year: 1962, 2008, 2006 Ill., maps (some color), photographs; Includes fiscal year financials, maps, photographs, agricultural economics and crop yield, some grazing financial information with cost of water usage, tables for irrigation and drainage and water storage and distributions, list of steam gaging stations, weather conditions, list of evaporation stations, quality of irrigation water at pumping plants, etc.; Title covers: calendar years for 1954-1962; Description is based on: Annual project history: Klamath Project, Oregon-California 1954; Dates of the beginning year(s) of publication are derived from May 1, 1903 to December 31, 1912, History of the Klamath Project and from the volume information on later volumes (v. 35) Klamath District and Klamath Project annual history for 1945, dated December 1, 1946 Title: Annual project history: Klamath Project, Oregon-California, 1962 Author: United States. Bureau of Reclamation Year: 1962, 2008, 2006 Ill., maps (some color), photographs; Includes fiscal year financials, maps, photographs, agricultural economics and crop yield, some grazing financial information with cost of water usage, tables for irrigation and drainage and water storage and distributions, list of steam gaging stations, weather conditions, list of evaporation stations, quality of irrigation water at pumping plants, etc.; Title covers: calendar years for 1954-1962; Description is based on: Annual project history: Klamath Project, Oregon-California 1954; Dates of the beginning year(s) of publication are derived from May 1, 1903 to December 31, 1912, History of the Klamath Project and from the volume information on later volumes (v. 35) Klamath District and Klamath Project annual history for 1945, dated December 1, 1946

1586. [Image] Hydrology of Crater, East and Davis Lakes, Oregon


	ill.; "With a section on chemistry of the lakes by A.S. Van Denburgh;" "Studies of water-budget balance in volcanic terranes for three lakes without surface outlets;" Includes bibliographical references ...
	Citation Citation Citation Abstract Copy Title: Hydrology of Crater, East and Davis Lakes, Oregon Author: Phillips, Kenneth N., b. 1897 Year: 1968, 2008 ill.; "With a section on chemistry of the lakes by A.S. Van Denburgh;" "Studies of water-budget balance in volcanic terranes for three lakes without surface outlets;" Includes bibliographical references (p. 44-45) and index Title: Hydrology of Crater, East and Davis Lakes, Oregon Author: Phillips, Kenneth N., b. 1897 Year: 1968, 2008 ill.; "With a section on chemistry of the lakes by A.S. Van Denburgh;" "Studies of water-budget balance in volcanic terranes for three lakes without surface outlets;" Includes bibliographical references (p. 44-45) and index

1587. [Image] Oversight field hearing on the Endangered Species Act 30 years later : the Klamath Project : oversight field hearing before the Subcommittee on Water and Power of the Committee on Resources, House of Representatives, One Hundred Eighth Congress, second session, Saturday, July 17, 2004, in Klamath Falls, Oregon


	"Serial no. 108-104."
	Citation Citation Citation Abstract Copy Title: Oversight field hearing on the Endangered Species Act 30 years later : the Klamath Project : oversight field hearing before the Subcommittee on Water and Power of the Committee on Resources, House of Representatives, One Hundred Eighth Congress, second session, Saturday, July 17, 2004, in Klamath Falls, Oregon Author: United States. Congress. House. Committee on Resources. Subcommittee on Water and Power Year: 2005 "Serial no. 108-104." Title: Oversight field hearing on the Endangered Species Act 30 years later : the Klamath Project : oversight field hearing before the Subcommittee on Water and Power of the Committee on Resources, House of Representatives, One Hundred Eighth Congress, second session, Saturday, July 17, 2004, in Klamath Falls, Oregon Author: United States. Congress. House. Committee on Resources. Subcommittee on Water and Power Year: 2005 "Serial no. 108-104."

1588. [Image] Klamath River basin : reclamation met its water bank obligations, but information provided to water bank stakeholders could be improved


	"March 2005." ; "GAO-05-283."
	Citation Citation Citation Abstract Copy Title: Klamath River basin : reclamation met its water bank obligations, but information provided to water bank stakeholders could be improved Author: United States. Government Accountability Office Year: 2005 "March 2005." ; "GAO-05-283." Title: Klamath River basin : reclamation met its water bank obligations, but information provided to water bank stakeholders could be improved Author: United States. Government Accountability Office Year: 2005 "March 2005." ; "GAO-05-283."

1589. [Image] Sediment oxygen demand in Upper Klamath and Agency Lakes, Oregon, 1999


	SIGNIFICANT FINDINGS The distribution of SOD2q values (measured sediment oxygen demand values corrected to 20°C [degrees Celsius]) had a median value of 1.6 g/m2/day (grams per square meter per day) in ...
	Citation Citation Citation Abstract Copy Title: Sediment oxygen demand in Upper Klamath and Agency Lakes, Oregon, 1999 Author: Wood, Tamara M. Year: 2001, 2005, 2004 SIGNIFICANT FINDINGS The distribution of SOD2q values (measured sediment oxygen demand values corrected to 20°C [degrees Celsius]) had a median value of 1.6 g/m2/day (grams per square meter per day) in the spring and 1.7 g/m2/day in the late summer. These values were well within the range of values in the literature for sites with similar sediment characteristics: primarily silty with at least a moderate amount of organic content. Over most of the lake there appears to be relatively little variation in SOD 14the interquartile range in values was 0.4 g/m2/day in the spring and 0.7 g/m2/day in the late summer. A significant exception was apparent in Ball Bay, where SOD in the late summer was greater than 10.2 g/m2/day. In the absence of primary production, an SOD of this magnitude could deplete the water column of oxygen in a few days. This measurement provided evidence that localized areas of very high SOD occur episodically in the bays, perhaps associated with large algal mats being trapped by the lake circulation patterns. A statistical test for a spring to late summer difference in the median values of SOD confirmed that SOD in the late summer (median value 1.7 g/m2/day) was significantly higher than in the spring (median value 1.2 g/m2/day). The difference was primarily due to seasonal changes in temperature; when SOD values were corrected to 20°C, there was no seasonal difference in the median values. There was no correlation between SOD20 and the sediment characteristics measured in this study: percent fines, organic carbon, and residue lost on ignition. Title: Sediment oxygen demand in Upper Klamath and Agency Lakes, Oregon, 1999 Author: Wood, Tamara M. Year: 2001, 2005, 2004 SIGNIFICANT FINDINGS The distribution of SOD2q values (measured sediment oxygen demand values corrected to 20°C [degrees Celsius]) had a median value of 1.6 g/m2/day (grams per square meter per day) in the spring and 1.7 g/m2/day in the late summer. These values were well within the range of values in the literature for sites with similar sediment characteristics: primarily silty with at least a moderate amount of organic content. Over most of the lake there appears to be relatively little variation in SOD 14the interquartile range in values was 0.4 g/m2/day in the spring and 0.7 g/m2/day in the late summer. A significant exception was apparent in Ball Bay, where SOD in the late summer was greater than 10.2 g/m2/day. In the absence of primary production, an SOD of this magnitude could deplete the water column of oxygen in a few days. This measurement provided evidence that localized areas of very high SOD occur episodically in the bays, perhaps associated with large algal mats being trapped by the lake circulation patterns. A statistical test for a spring to late summer difference in the median values of SOD confirmed that SOD in the late summer (median value 1.7 g/m2/day) was significantly higher than in the spring (median value 1.2 g/m2/day). The difference was primarily due to seasonal changes in temperature; when SOD values were corrected to 20°C, there was no seasonal difference in the median values. There was no correlation between SOD20 and the sediment characteristics measured in this study: percent fines, organic carbon, and residue lost on ignition.

1590. [Image] The Endangered Species Act and the National Research Council's interim judgment in Klamath Basin


	The controversial 2001 U.S. Fish and Wildlife Service water allocation decision in the Klamath Basin has been portrayed as an example of scientific guesswork operating under a flawed Endangered Species ...
	Citation Citation Citation Abstract Copy Title: The Endangered Species Act and the National Research Council's interim judgment in Klamath Basin Author: Cooperman, Michael S. ; Markle, Douglas F. Year: 2002, 2005 The controversial 2001 U.S. Fish and Wildlife Service water allocation decision in the Klamath Basin has been portrayed as an example of scientific guesswork operating under a flawed Endangered Species Act. This conclusion has been based on an interim National Research Council report, quickly prepared in late fall, 2001. We have reviewed several iterations of the NRC Interim Report as well as all Biological Opinions and management documents related to Klamath Basin suckers and provide an overview. The 2001 Biological Opinion and the Interim Report illustrate the lack of consensus typical of scientists in the early stages of exploring a complex system. Unfortunately, the decision created hardship for a small group of people and the lack of scientific consensus has politicized the debate. Politicians have assumed that the Interim Report has primacy in the scientific debate when, in fact, its speedy construction contributed to multiple errors that detract from its scientific usefulness. The NRC Interim Report has, instead, primarily served to deflect debate away from the needs of listed fishes to one about shortcomings in the Endangered Species Act. Although the process of science has been served by both the 2001 Biological Opinion and the Interim Report, both have shortcomings, and we see no justification for either side labeling the other's decisions or conclusions as "not sound science." Title: The Endangered Species Act and the National Research Council's interim judgment in Klamath Basin Author: Cooperman, Michael S. ; Markle, Douglas F. Year: 2002, 2005 The controversial 2001 U.S. Fish and Wildlife Service water allocation decision in the Klamath Basin has been portrayed as an example of scientific guesswork operating under a flawed Endangered Species Act. This conclusion has been based on an interim National Research Council report, quickly prepared in late fall, 2001. We have reviewed several iterations of the NRC Interim Report as well as all Biological Opinions and management documents related to Klamath Basin suckers and provide an overview. The 2001 Biological Opinion and the Interim Report illustrate the lack of consensus typical of scientists in the early stages of exploring a complex system. Unfortunately, the decision created hardship for a small group of people and the lack of scientific consensus has politicized the debate. Politicians have assumed that the Interim Report has primacy in the scientific debate when, in fact, its speedy construction contributed to multiple errors that detract from its scientific usefulness. The NRC Interim Report has, instead, primarily served to deflect debate away from the needs of listed fishes to one about shortcomings in the Endangered Species Act. Although the process of science has been served by both the 2001 Biological Opinion and the Interim Report, both have shortcomings, and we see no justification for either side labeling the other's decisions or conclusions as "not sound science."

1591. [Image] Klamath Falls Resource Area Planning Update, Winter 2003


	U. S. Die artment sf the Interior Bu. rea. u oP L and Management K I W ~ Falls R~& G urnw . 2795 & tdeaonAvepue, BuMng #% Klamath F~ HSO, r egon 97803 . . January 2004 Klamath Falls Resource Area Planning ...
	Citation Citation Citation Abstract Copy Title: Klamath Falls Resource Area Planning Update, Winter 2003 Author: United States. Bureau of Land Management. Klamath Falls Resource Area Office Year: 2003, 2004 U. S. Die artment sf the Interior Bu. rea. u oP L and Management K I W ~ Falls R~& G urnw . 2795 & tdeaonAvepue, BuMng #% Klamath F~ HSO, r egon 97803 . . January 2004 Klamath Falls Resource Area Planning Update Winter 2003 United States Department of the Interior BUREAU OF LAND MANAGEMENT Klamath Falls Resource Area 2795 Anderson Avenue, Building 25 Klarnath Falls, Oregon 97603- 7891 Phone: ( 541) 883- 6916 1 Fax: ( 541) 884- 2097 E- Mail Address: Username@ or. blm. gov Website: http: llwww. or. blrngov/ L. akeview/ kfra/ index. htrn KLAMATH FALLS RESOURCE AREA PLANNING UPDATE Winter 2003 The primary purpose of this Planning Update is to inform you about the activities on the Klarnath Falls Resource Area. It is my desire to keep you informed about issues, activities, and opportunities I think are important to the public. More importantly, I am seeking ideas and comments from those who may be affected by multiple- use management programs here on the resource area. This planning update is organized to make it easy for you to find projects of most interest. Projects have been arranged into categories ( i. e., Recent Decisions, New Projects, On- going Projects, and Environmental Education Activities). In addition, each of these categories is sorted by resource topics ( e. g., Lands Program, Timber Sales, etc.). The table will give you a brief description of activities occurring within the Klamath Falls Resource Area and for most projects a location. Refer to one of three maps following the table, for locations of projects. Additional information can be obtained fi- om the contact listed in the project descriptions. If you have any concerns about the proposed actions, please call the Klarnath Falls Resource Area and ask for the " Contact" person listed or the Resource Area Planner as soon as possible. The earlier you get involved, the more capability we have to adjust or change planned actions. Also be alert for news releases and public notices published in the Herald and News as projects reach stages for public involvement. If you want to provide comments to a specific environmental assessment, please send or deliver your written comments addressed to the Field Manager, Klamath Falls Resource Area, by the close of, or postmarked by the last day of the comment period. Your comments and concerns are welcomed, and could influence the final decision on these projects. I would appreciate any comments or suggestions you may have regarding this p l h i n g update or how it could be improved to make it more useful to you. Thank you for your continued interest in BLM's management of public lands. If you have any questions on this planning update, stop by the office or call ( 541) 883- 6916. Jon Raby, Field Manager Klamath Falls Resource Area BUREAU OF LAND MANAGEMENT ' KLAMATH FALLS RESOURCE AREA 2795 ANDERSON AVENUE, BLDG. # t5 KLAMATH FALLS, OR 97603 PHONE NUMBER: ( 541) 883- 6916 MAP PROJECT TITLE & DESCRIPTION LOCATION SPECIAL AREAS STATUS OF COMPLETION CONTACT REF. # AFFECTED ANALYSIS DATE CX = Categorical Exclusion, DNA = Determination of NEPA Adequacy, EA = Environmental Assessment, EIS = Environmental Impact Statement Klarnath Falls Resource Area, Winter 2003 Planning Update - Page 2 New Projects - Watershed Map # 4 T39S. R14E, Secs. 10, 11,14, 15 Norcross Vegetation Treatments - Thin ponderosa pine, remove invasive juniper, restore native vegetative communities ( grass, shrub, pine), and monitor the effects of treatment on vegetative and hydrologic resources. New Projects - Roads and Facilities None Map 1 EA in progress. Road crossing Spencer Creek Spencer Creek Culvert Replacement Spencer Watershed Riparian Fence Reconstruction New Projects - Recreation I Topsy Recreation Site Improvements - Campground water 1 T40S, R7E, Sm. 1 Map # I0 1 system and boat ramp improvements None I DNAS~ nnrrr2004 I Fall 2005 New Projects - Range Management Fall 2007 Fish passage Riparian Protection Mike Turaski in progress CX in progress Map #' DNA Spring 2004 Pitch Log Creek, Long Branch Creek, and Antelope Creek within the Gerber Block Gerber Watershed Riparian Fencing - Emposed project to construct livestock exclosure fencing along about 1.1 miles of Pitch Log Creek, 1.5 miles of Long Branch Creek, and 1.7 miles of Antelope Creek. Maintain fences as riparian exclosures or riparian pastures. Monitor effects of reduced livestock use on vegetation and streambank conditions. New Projects - Timber Management Contract - Fall 2004 Construction - 2005. Summer 2004 Riparian protection Fall 2004 Andy Hamilton Andy Hamilton Dana Eckard Jenny Creek Watershed South Gerber Block Jenny Creek Watershed South Gerber Block I I I None 1 None Jenny Creek EA - Purpose of this EA is to address a variety of forest health and restoration treatments in the Jenny Creek Watershed. Proposed treatments may include; commercial timber sales, non- commercial silvicultural treatments, riparian restoration treatments, aspen stand restoration and road restoration projects. South Gerber EA - Purpose of this EA is to address a variety of forest health and restoration treatments in the South Gerber Block area. Proposed treatments may include; commercial timber sales, non- commercial silvicultural treatments, riparian restoration treatments, juniper woodland treatments, aspen stand restoration and road restoration projects. LOCATION Recent Decisions - Lands Program 1 I I I I I Upper Spencer Creek Road Treatments - Road Upper Spencer Creek I' Implementation in July obliteration, decommissioning, realignment, improvement, T38S, R6E Sections Riparian Resenres DDRBs I 2M Mike Turaski and stream crossing removal. 15 and 23 12123103 Recent Decisions - Wildlife M Map 1 # 43 ecisions - Waters Map 1 # 21 Willow Valley Habitat Enhancement Willow Valley Warm water fishexies Implementation pending Reservoir ODFW involvement. Section 1 Exploration Quarry Expansion Drilling - Authorization for ODOT to conduct exploratory drilling in and around an existingpit to identify a source for additional mineral material. Scott Snedaker I I I I I I Recent Decisions - Fuels Treatment T40S, R6E, Sec. 1. N112NW114 Map 1 # 3 None Boundary Springs Yarding and Removal of Cut Juniper - Purpose of this project is to remove juniper boles in previously treated areas to reduce fuel accumulation and promote commercial use of juniper. None Ben Hall 1 & 2, Cerber Potholes, Sehnipps, and FIZ 95- 71 Juniper Yarding - to remove juniper boles in previously treated areas to reduce fuel accumulation and promote commercial use of juniper. Fint 360 acres yarded and material sold to Area FTZ- 1 04 utilization local mill ( REACH) that utilizes juniper. Exploration initiated as weather permits. Rebecca La& Linda Younger Mike Bechdolt Various Mike Bechdolt Klamath Falls Resource Area, Winter 2003 Planning Update - Page 3 Fuel treatment, juniper utilization DNA completed. Project on hold. BUREAU OF LAND MANAGEMENT KLAMATH FALLS RESOURCE AREA AVEl PHONE NUMBER: 2795 ANDERSON AVENUE, BLDG. # 25 ' E ( 541) 8836916 SPECIAL AREAS STATUS OF AEFECrED ANALYSIS PROJECT TITLE & DESCRIPTlON LOCATION AEFErnD COMPLETION DATE CONTACT r~ ann~ ng~ na~ ysis~ lrnp~ ernen- r Gareinoenr al RMP Evaluation~ Revision- In the final settlement agreement to the American Forest Resource Council vs. Bureau of Land Management ( BLM) litigation, the BLM is directed to revise Resource Management Plans ( RMPs) in western Oregon by December, 2008. The BLM began the revision process in 2003, evaluating current plans and developing a project preplan. Project status information will be posted on the District website. Formal scoping is expected in the second half of calendar year 2004. RMP Revision - FY 2008 None Resource Area Wide All Resources Evaluation in progress Don Homeins GerberlWillow Valley Coordinated Resource Management Plan ( CRMP) Watershed Analysis. - A local planning team of private landowners, StatelFederal land managers, and concerned citizens recommends future project implementation on private land in CRMP area. CRMP meetings/ discussions are continuing Map 1 # 5 GerberNillow Valley Watershed Completion date open-Rivate Lands ended Don Homeins Lany Frazier Wild and Scenic River designation, Area of Critical Concern, T& E spp. Map l # 28 Upper Klamath River Management Plan DEE - Develop a management plan in response to Wild and Scenic Riven Act requirements for river segment approx. 20 miles long encompassing 6,400 acres. Klarnath River - J. C. Boyle Reservoir, Oregon, to Copco One Reservoir, California Draft EIS released 511 612003. Comment period closed 8/ 13/ 2003. FEIS December 2004 Upper Klamath Basin and Wood River Wetland Resource Management Plan Amendment for the Fourmile Creek portion of this area. The purpose of this project is to amend the Upper Klamath Basin and Wood River Wetland RMP EIS to designate the Fourmile Creek area as an Area of Critical Environmental Concern. Riparian Wetland Area of Critical Environmental Concern ( ACEC) Draft EIS to be prepared. Specific schedule and completion date unknown. ACEC Evaluation submitted to District Manager, October 2000. Map 1 # 29 Fourmile Creek Wetland Lou Whiteaker Lany Frazier Draft MOU presented to the Tribal Council on 2/ 22/ 2000. Waiting for Tribal feedback. - -- Unknown Memorandum of Understanding ( MOU) between the Klamath Tribes and BLM for Coordination on Management Issues. - The proposed MOU identifies a process to coordinate tribal involvement with BLM management actions on public lands. Late- Successional Reserve ( LSR) Assessment. A single LSR Assessment was prepared to assess all 19 Unmapped LSRs designated within the resource area and develop management recommendations for these areas to restore or maintain late successional habitat. Former Tribal None Lakeview District Lands - None Draft submitted to and pending approval from the Regional Ecosystem Office ( REO). BLM lands west of Highway 97 covered by the Northwest Forest Plan Unmapped Late Successional - Reserves. Analysis is complete. - ou Whiteaker Klamath Falls Resource Area, Winter 2003 Planning Update - Page 4 2795 ANDERSON AVENUE, BLDG. # 25 KLAMATH FALLS, OR 97603 541) 8834916 STATUS OF COMPLETION DATE CONTACT AFFECTED I ANALYSIS I - Map 2 # 46 - None Map 1 -# 7 Map 1 # 22 - None Map 2 # 44 Map 2 # 30 Oak Thinning - Thin 100 acres of oak woodland to restore plant communities and reduce potential for stand replacing wildfires and overall fire management costs. Noxious Weed Treatments - contain1 reduce noxious weed populations using integrated pest management ( manual, mechanical, chemical, and biological control methods). Activities tier to KFRA Integrated Weed Control Plan ( IWCP) and EA- OR- 014- 93- 09 approved July 21, 1993. T40S, R6E, Sec. 35 T41S, R6E, Sec. 3 and 10 T41S, WE, Sec. 1 Weed- infested sites throughout the Klamath Falls Resource Area Bitterbrush Planting - - Various locations Ongoing Planning/ Analysisflmplementation - Vegetation Treatments I I I -- -- - Horton Rim I Windy Ridge Juniper Removal - Juniper treatment for fuel reduction and wildlife habitat inmovement GerberlWillow Valley Riparian Conifer Treatments - removing invasive juniper from riparian areas in the Gerber Block G& I Willow Valley Watersheds Spencer Creek Riparian Thinning- thin 80 acres of iuniverlmixed conifer T38S, R6E, Secs. 21 and 28 Clover Creek DDRB - 108 acres mechanical treatment. T. 38S, R6E, Sec. 27.34 Off Spencer Hookup Road I Document is tiered to the Northwest Area Noxious 1 Noxious Weed I Klamath River canyon/ ACEC None I Wyd Control Program Treatments occur May - EIS avvroved December I October on a vearlv I Lou mitaker Analysis in Progress. 1985: supplemented in March 1987. Analysis completion expected Spring 2004. - . basis. Mule deer winter range. Rob Roninger None I EA completed Riparian Reserves EA completed. I Ongoing - Possible in Key Watershed completion in 2004 I Mike Turaski cx completed. h j e c t in progress. Riparian, critical sucker habitat 2- 3 year implementation began Spring 2003. Ongoing Planning/ Analysis/ Implementation- Lands Treatments occur on a yearly basis. Hapa DNA completed. Bald Eagles, Survey and Manage species Map l # 8 Greg Reddell Map 1 # 17 Implementation initiated 2003 - Ongoing DNA completed in Spring 2001. Mike Turaski Map I -# 20 Map 1 -# 9 On hold for RE0 approval of LSRA - ~- - Dehlinger Trust - Residential Road ROW and easement. Bmner Land Exchange Steve Haper Bly Dump Sale ( EA No. OR- 014- 97- 01) - Purpose of # l8 this project is to sell Bly Transfer Station to Klamath Co. I of Bly'OrrgOn. Map I I None Known I Analysis in progress I Winter2004 Linda Younger T40S, RIOE, Sec. 9 South Bryant Mountain Al B ~ n eLra nd Sale Nancy Charley Trust Reciprocal Easement and ROW Klamath Falls Resource Area, Winter 2003 Planning Update - Page 5 None Unknown T41S, R13E. Sec. 14 T38S, RSE, Sec 12- 13 Reciprocal Easement Pending On hold Unknown Borders Riparian Reserve Winter 2004 Spring 2005 EA completedl Decision record pending CX completed, easement pending Linda Younger Linda Younger Spring 2004 Fall 2004 Linda Younger Linda Younger MAP PROJECT TITLE & DESCRIPTION REF. SPECIAL AREAS IC OMPLI AFFECTED Ongoing Planning/ Analysis/ Imp LOCATION ETION DATE I COMA dementation - rimber Sales I - - - Non - Non Roaming Salvage EA - The purpose is to provide NEPA coverage for timely salvage of timber mortality over the entire Resource Area. Entire Resource Area Unknown Preparing scoping letters. Spring 2004 I MI* cBechdo1t FY 04 - Baldy Salvage Timber Sale - Sale is designed to harvest windthrown trees as a result of 2003- 4 windstorms and scattered insect and disease related mortality. Anticipated volume is I . O- 1 SMMBF on 300- 500 acres. FY 04 - Matchbox Title I1 Service Contradl'imber Sale - The project consists of a Forest Health Density ManagementIUnderstory Thinning of overstocked mixed conifer stands. The sale is being designed under the Secure Rural Schools and Community Self- Determination Act of 200 - Public Law 106- 393. A service contract will be used to thin, yard, and deck trees from an overstocked mixed conifer stand. A timber sale contract will be used sell the decked material. Approximately 300 acres are scheduled for treatment resulting in about 600 MBF. Primarily in the Surveyor Mtn and Burton Butte Areas. May also include some eastside areas. Timber Sale is scheduled to be sold in Mike Bechdolt May or June of 2004 Presently marking some of the scatted salvage Matrix Contract is scheduled to be awarded in June or Mike Bechdolt July of 2004 Chase Mountain Area T. 40S., R. 7E., Sec. 9 Presently Preparing the Matrix Timber Sale Contract Proposed sale date: Summer 2005 Mike Bechdolt Riparian Reserves T38S., ME., Sec. l3,15,23, 25 and 26 Reserves! Matrix Buck Again Timber Sale - An estimated 700 acres is designed for treatment in the Spencer Creek watershed near Buck Lake. Approx. 4 MMBF to be harvested. Sale preparation. Chew Timber Sale- Approximately 1,000 acres density management understory reduction adjacent to and south of T40S. R6E, Secs. 1, 1 1,14 T40S, R7E. Secs. 3 and 5 Proposed sale date Mike Bechdolt Hwy 66 west of la math Falls. ~ aleanal~ zuendd er the Sale preparation. Spring 2004 or 2005. Topsy/ Pokegama/ Hamaker EA (# OR- 0 14- 98- 01 ). Estimated volume of 2.5 m b f . None Oneoine Plannine/ Analvsis/ Implementation - Roads and Facilities Map 1 # 77 Map # 73 Klamath Falls Resource Area, Winter 2003 Planning Update - Page 6 Sediment Traps - 30 sediment traps on BLM, USFS, and private land Map I # 6 Gcrber Road Sediment Reduction - road resurfacing and drainage improvement to reduce sediment delivery to streams in the Gerber Watershed Spencer Creek Watershed and Gerber Block Gerber Washrack- Installation of facility at Gerber Guard Station for washing equipment to control the suread of noxious weeds and overhead filling of tankers. 5 stream crossings None Gerber Guard Station Critical sucker habitat DNA completed. Sediment traps installed. Noxious weed prevention EA completed. Implementation initiated I Fall 2004 Monitoring in progress. Mike Turaski CX completed. Mike Turaski Pending funding. Bob Crumrine/ Brian McCarty - I - 1 - Map 1 # 6 Ongoing Planning/ Analysis/ Implementation - Roads and Facilities ( continued) Gerber Area Recreation Improvements - ( RMP ROD EIS 6- 2- 95, pp. 49- 50) - Project falls under corrective maintenance, improvement or replacement in the Klamath Falls RMP. Existing maintenance, improvement or replacement include: rocking and chip- sealinglpaving road system and campsites, picnic tables, barrier posts, camp host RV holding tank, hydrants, Barnes Valley Boat Ramp access road. Scott Smter Gerber Reservoir Recreation Site Gerber Area Primitive Camp and Day Use Sites Recreation Improvements. The objectives of these improvements are to update or improve existing facilities to continue to provide an enhanced recreational experience and satisfy visitor needs. T& ESpecies ( suckers and bald eagles) Scott Senter Stan H Spring, Potholes, Miller Creek, Frog Camp, Pitchlog Creek, Wildhorse, Basin, Rock Creek and Willow Valley Reservoir Map l # 6 Projects in compliance GththeKFIURMP. Determination of NEPA Adequacy completed and approved on 10128199. Wood River Wetlands Project - Remaining projects: Finish installation of fish screen on 7- mile Canal diversion structure and floating boardwalk, interpretive signs, and trail system. Surface rock dike roads from bridge to 7- mile Canal and add group interpretive site. Juniper Chip Road - Using juniper debris for biomass or by- product in Oshea ( mZ 95/ 71), and Norcross Springs. FY 2004 - Miller Creek- Potholes trail to be constructed T& E Species ( suckers) wood River Property I I Upper Klamath Basin and Wood River Wetland I A Determination of NEPA Adequacy ( DNA) completed 9/ 25/ 2000. ( Project contingent on funding) Map 1 # 25 - Map 2 # 70 FY 2004- sidewalks and pinic tables to be installed at Willow Valley Res. Wedge Watkins Joe Foran 25 miles north of Klamath Falls, Oregon T 39 8 40s. R13,14,14XE I None Known I I Stewardship contract EAcompIeted being developed. Ongoing Projects - Prescribed Burning and Fuels Treatment Wetlands Map 2 # 2 Resource Management Plan EIS; decision signed June 16,1995. Joe Foran Pending funding Short Lake Broadcast Bum - Prescribe bum approx. 280 acres outside FTZ to reduce fuel loading and risk of wildfire. T38S. R1 I E, Sec 20 & 29 - - - - - - -- - - - - - Miller Creek Mechanical Treatment - Proposal to use mechanical piling instead of prescribed buming of a~ oroximatelv I00 acres. Map 2 # 37 - T39S. R13E. Sec. 14 & 23 Analysis Completed ACEC 1 FONSl and Decision Record on 3- 24- 99. Joe Foran None Known Project delayed. EA completed Fuels Maintenance Treatments # t ( KCER - 00- 03) Treat approximately 1,200 acres to remove fire- prone brush, excessive levels of hazardous fuels ( less than 6" in diameter), and small conifers that are ladder fuels and threats to over stow trees bv crown fire.. Map 2 # I 1 Spring 2004 Klamath Falls Resource Area, east of Hwy 97. See Prescribed Fire Map for locations. None Known Dale Brush Map 2 # 62 Analysis completed. Multiple year implementation - ongoing. Mechanical Slash Treatment Project - Mechanical treatments ( shearing, chipping, or grinding) to reduce fuels and control vegetation on approx. 12,000 acres. Joe Foran Multiple Locations Resource Area Wide None / Second DNA completed. Klamath Falls Resource Area, Winter 2003 Planning Update - Page 7 Projects tasked out over a three year period - ongoing. PROJECT K. 1 TITLE & DESCRIPTIO SPECIAL AREAS STATUS OF 4 CONTACT AFFECTED ANALYSIS - Map 2 -# 39 Map 2 # 40 - Map 2 -# 42 Map 2 # 38 Map 2 # 63 Map 2 # 64 - Map 2 # 65 & # I9 Map 2 # 45 - Map 2 # 49 - Stukel98- 1 Mechanical Treatment - Mechanical piling T40S, RIOE, Sec. 10,11,14, instead of pmcribed burning of approximately 500 acres. 23,24 Stukel98- 2 Prescribed Burn - Prescribe bum approx. 3,000 acres to: Reintroduce fire to restore plant communities, while reducing the potential for stand-replacement wildfires and overall fire management costs. T40S, RIOE, Sec. 12,13,24 T40S, RllE, Sec. 7& 18 HamakerIChase Fuels Treatment - Reduce Fuels on T40S, R8E 4000 acres south of Hwy 66 I Stiles Spring Prescribed Burn - Project purpose to bum approximately 1,000 acres to: Reinduce fire to restore sustainable function and structure to plant communities, while reducing the potential for stand- replacement wildfires, and reducing overall fire management costs. Stukel98- 7 & 9 Prescribed Burns - Prescribe bum approximately 525 acres to: reintroduce fire to restore plant communities, reduce overall fire management costs and the potential for stand- replacing wildfires. Statelinel Holbmk Prescribed Bums - Presmie bum approximately 4.000 acres to reduce fuel loading and risk of catastrophic wildfire. T37S, RIOE, Sec. 3- 5,9- 11, 14- 15 T40S, RllE, Sec5 & 6 T. 40S, R15 E., T. 41S, RISE. -- Big Adobe Prescribed Burn - Prescribe bum approximately 6,700 acres to reduce fuel loading and risk of catastrophic wildfire ( includes Wild Midway Rx Bum) Range- Juniper Treatment - Hazardous fuel reduction, T40S. R12E. Sec. 1 1 using mechanical and prescribed fire methods. T41 S, RISE Upper Swan Prescribed Burn - Project purpose: bum approximately 98 acres to restore sustainable function and structure to plant communities, reduce potential for stand-replacement wildfires and overall fire management costs. g and Fuels Treatment ( continued) None Known Project0 t1ie 4r- s9 4to- 0E9A. # OR- Project ongoing Joe Fmn T37S, RIOE, Sec. 24 & 25 T37S, RI 1.5E, Sec. 31 Bald Eagle ( Analysis Completed- I 200 acres treated in FY I None Analysis Completed Project tiers to EA # OR- 014- 94- 09. EA completed Wildlife Habitat Riparian Initiated Winter 2001 Fall 2004 Joe Foran Project delayed until the Spring 2004 Bald None Bald Eagle I Planned projects tier to the Promammatic Fire I Joe Foran Joe Foran Project initiated, 2- 3 year implementation FONSI - 12- 1 9- 99. 2000; Remainder Decision Record on 01 - 25- 2000 ,, Foran Joe Foran Analysis Completed Project tiers to EA # OR- 014- 94- 09) approved on 4- 29- 94. Initiated Winter 2001 Klamath Falls Resource Area, Winter 2003 Planning Update - Page 8 Wildlife forage/ habitat improvement 130 acres completed Remainder Spring 2004 Accomplished 1500 acres. Remainder Fall 2004. Steve Pehick- Underwood Joe Foran DNA completed ongoing 2- 3 year implementation Joe Foran .. " "" . 7 < .,.. - . . 7 - " b - . " < * - - ' 7 , 4 . , v ,-' w., ,. ' q"* -?, . x-.. s,... >,% VW? P ,.- 7i,- .. x., < 8 SCHEDULE OF PROPOSED PROJECTS BUREAU OF LAND MANAGEMENT KLAMATH FALLS RESOURCE AREA 2795 ANDERSON AVENUE, BLDG. # 25 KLAMATH FALLS, OR 97603 PHONE NUMBER: ( 541) 883- 69 MAP PROJECT TITLE & DESCRIPTION LOCATION I SPECIAL AREAS STATUS OF ANALYSIS COMPLETION CONTACT REF. # AFFECTED DATE Rangeland Health Standards Assessments - in progress I These assessments compare the monitoring information collected against the five Standards for Rangeland Health and propose management changes if current grazing use is not meeting the Standards, or not making significant improvement towards meeting them. Changes are implemented through the grazing decision or agreement process. z3I Re16 Allotment ( M893) I South Langell Valley I None Known I Assessment in progress I Summer 2004 I Dana Eckard M$\ 3 I KIamatL Forest Estates Allotment ( M862) 1 North of Bonanza -~ Yainax Allotment ( M861) I None Known I Assessment in progress I ~ ~ - 2 0 0 4 I Bill Lindsey North of Bonanza Map # 55 None Known ? G3 Haskins Allotment (# 0826) y&' Assessment in progress Masten Allotment ( M842) Map # 68 North of Bonanza Kellian Allotment (# 0834) Hungry Hollow Allotment (# 0830) Klamath Falls Resource Area, Winter 2003 Planning Update - Page 9 SUM 2004 North of Bonanza Adams Allotment (# 0800) Rangeland Health Standards Assessments - completed* Bill Lindsey None Known North of Bonanza North of Bonanza None Known East of Bonanza Bill Lindsey Assessment in progress None Known None Known * A total of 37 Rangeland Health Standards Assessments have been completed to date, 1 has been completed so far in FY 2004. Assessment in progress None Known None Known Assessment completed Summer 2004 Assessment in progress Assessment in progress Map North of Bonanza December 2003 # 48 Dana Eckard Summer 2004 Assessment in progress McCartie Allotment (# 0860) Dana Eckard Summer 2004 Summer 2004 Dana Eckard Summer 2004 Dana Eckard Dana Eckard Presentations/ Environmental Education Programs/ Tours ( Fiscal Year to Date) Fun With Fungi I 1 1/ 2/ 03 I Seven Mile Area Adults 25 I What Was Presented Overview of past and current outreach events; permit sales Wood River Wetland Field Trip Operation Indian Rocks ARPA Investigation 1 1 1/ 3/ 03 ( Central Washington University 1 Faculty and Students I 51 I Date 1 Group / Age # of People 1 01 1 5/ 03 10/ 28/ 03 Where Cultural Resource Management and the NEPA Process Archaeological Investigations in the Great Basin I Wildlife Management 1 12/ 16/ 03 1 OIT - " Expanding Horizons" I 8* Grade Students I 120 1 Ross Ragland Theater Wood River Wetland Coloring Books 1 1/ 3/ 03 1 1/ 4/ 03 Klarnath Falls Resource Area, Winter 2003 Planning Update - Page 10 Answer People/ Adults Oregon Institute of Technology Students I 1 1 11 9/ 03 Shasta Elementary School -- - S - 290 Fire Behavior 25 - 30 Central Washington University Central Washington University Elementary Students 30 12/ 20/ 03 Graduate Student Seminar Graduate Student Seminar 24 35 Klamth Community College Adults 8 EventIActivlty Date Location Contact( s) F 01 rarnclpanrs ( EmployeeslPublic) IBald Eagle Conference I Februaryl3- IS I Oregon Institute of Technology I Steve Haynerl Kelly Hollums I l~ arthD ay I April I Jefferson Square Mall I Greg Reddell I Klamath Watershed conference February 24 - 26 Wilderness & Horse Packing Clinic* International Migratory Bird Day IMBD Pre- event Classes -- - IMBD Educator Workshop Oregon Institute of Technology May ( IMBD) April 24 IMBD Event National Free Fishing Day RAP Camp Klamath County Fair Klamath Falls Resource Area, Winter 2003 Planning Update - Page 11 Wedge WatkinslKelly Hollums April 16 - pp - - Sixth Grade Forestry Tour National Public Lands Day Oregon Archeology Celebration Klarnath County Fairgrounds Klamath Community College May 8 June June August Tonya PinckneyIScott Senter Steve Hayner, et al OSU- Klamath Co. Extension * Numbers of public participants for large events are estimated. ** BOLD WRITING indicates that project is funded with District Outreach dollars. September September September Veteran's Park To Be Announced Camp Esther Applegate Klamath County Fairgrounds Steve Hayner, et al Steve Hayner Scott Snedaker To Be Announced PinckneylSenter Clover Creek Educational Area To Be Announced To Be Announced ~ p Bill Johnson To Be Announced Michelle Durant Glama th Falls Resource Area Miscellaneo~ wP roject Loca ticms R6E RBE R7E RBE RBE RlOE RIIE R12E R13E R14E R14.6E R16E Klamath Falls Resource Area, Winter 2003 Planning Update - Page 12 N LEGEND R5E R6E R7E R8E RQE RIOE R l l E R12E R13E R14E R14.5E R15E Klarnath Falls Resource Area, Fall 2003 Planning Update - Page 13 UNITED STATES DEPARTMENT OF THE INTERIOR BUREAU OF LAND MANAGE~ ENT Klarnath Falls Resource Area Office 2395 Parderson Avenue, Building a 5 Kfamth MIS. Oregan 97603 OF. FIGIAL, BUSI~ ESS PENALTY FOR PRIVATE USE, $ 300 Marita Kunkel Library Director Oregon Institute of Techolagy 3201 Cempus Dr Klamath Falls, OR 97601 Title: Klamath Falls Resource Area Planning Update, Winter 2003 Author: United States. Bureau of Land Management. Klamath Falls Resource Area Office Year: 2003, 2004 U. S. Die artment sf the Interior Bu. rea. u oP L and Management K I W ~ Falls R~& G urnw . 2795 & tdeaonAvepue, BuMng #% Klamath F~ HSO, r egon 97803 . . January 2004 Klamath Falls Resource Area Planning Update Winter 2003 United States Department of the Interior BUREAU OF LAND MANAGEMENT Klamath Falls Resource Area 2795 Anderson Avenue, Building 25 Klarnath Falls, Oregon 97603- 7891 Phone: ( 541) 883- 6916 1 Fax: ( 541) 884- 2097 E- Mail Address: Username@ or. blm. gov Website: http: llwww. or. blrngov/ L. akeview/ kfra/ index. htrn KLAMATH FALLS RESOURCE AREA PLANNING UPDATE Winter 2003 The primary purpose of this Planning Update is to inform you about the activities on the Klarnath Falls Resource Area. It is my desire to keep you informed about issues, activities, and opportunities I think are important to the public. More importantly, I am seeking ideas and comments from those who may be affected by multiple- use management programs here on the resource area. This planning update is organized to make it easy for you to find projects of most interest. Projects have been arranged into categories ( i. e., Recent Decisions, New Projects, On- going Projects, and Environmental Education Activities). In addition, each of these categories is sorted by resource topics ( e. g., Lands Program, Timber Sales, etc.). The table will give you a brief description of activities occurring within the Klamath Falls Resource Area and for most projects a location. Refer to one of three maps following the table, for locations of projects. Additional information can be obtained fi- om the contact listed in the project descriptions. If you have any concerns about the proposed actions, please call the Klarnath Falls Resource Area and ask for the " Contact" person listed or the Resource Area Planner as soon as possible. The earlier you get involved, the more capability we have to adjust or change planned actions. Also be alert for news releases and public notices published in the Herald and News as projects reach stages for public involvement. If you want to provide comments to a specific environmental assessment, please send or deliver your written comments addressed to the Field Manager, Klamath Falls Resource Area, by the close of, or postmarked by the last day of the comment period. Your comments and concerns are welcomed, and could influence the final decision on these projects. I would appreciate any comments or suggestions you may have regarding this p l h i n g update or how it could be improved to make it more useful to you. Thank you for your continued interest in BLM's management of public lands. If you have any questions on this planning update, stop by the office or call ( 541) 883- 6916. Jon Raby, Field Manager Klamath Falls Resource Area BUREAU OF LAND MANAGEMENT ' KLAMATH FALLS RESOURCE AREA 2795 ANDERSON AVENUE, BLDG. # t5 KLAMATH FALLS, OR 97603 PHONE NUMBER: ( 541) 883- 6916 MAP PROJECT TITLE & DESCRIPTION LOCATION SPECIAL AREAS STATUS OF COMPLETION CONTACT REF. # AFFECTED ANALYSIS DATE CX = Categorical Exclusion, DNA = Determination of NEPA Adequacy, EA = Environmental Assessment, EIS = Environmental Impact Statement Klarnath Falls Resource Area, Winter 2003 Planning Update - Page 2 New Projects - Watershed Map # 4 T39S. R14E, Secs. 10, 11,14, 15 Norcross Vegetation Treatments - Thin ponderosa pine, remove invasive juniper, restore native vegetative communities ( grass, shrub, pine), and monitor the effects of treatment on vegetative and hydrologic resources. New Projects - Roads and Facilities None Map 1 EA in progress. Road crossing Spencer Creek Spencer Creek Culvert Replacement Spencer Watershed Riparian Fence Reconstruction New Projects - Recreation I Topsy Recreation Site Improvements - Campground water 1 T40S, R7E, Sm. 1 Map # I0 1 system and boat ramp improvements None I DNAS~ nnrrr2004 I Fall 2005 New Projects - Range Management Fall 2007 Fish passage Riparian Protection Mike Turaski in progress CX in progress Map #' DNA Spring 2004 Pitch Log Creek, Long Branch Creek, and Antelope Creek within the Gerber Block Gerber Watershed Riparian Fencing - Emposed project to construct livestock exclosure fencing along about 1.1 miles of Pitch Log Creek, 1.5 miles of Long Branch Creek, and 1.7 miles of Antelope Creek. Maintain fences as riparian exclosures or riparian pastures. Monitor effects of reduced livestock use on vegetation and streambank conditions. New Projects - Timber Management Contract - Fall 2004 Construction - 2005. Summer 2004 Riparian protection Fall 2004 Andy Hamilton Andy Hamilton Dana Eckard Jenny Creek Watershed South Gerber Block Jenny Creek Watershed South Gerber Block I I I None 1 None Jenny Creek EA - Purpose of this EA is to address a variety of forest health and restoration treatments in the Jenny Creek Watershed. Proposed treatments may include; commercial timber sales, non- commercial silvicultural treatments, riparian restoration treatments, aspen stand restoration and road restoration projects. South Gerber EA - Purpose of this EA is to address a variety of forest health and restoration treatments in the South Gerber Block area. Proposed treatments may include; commercial timber sales, non- commercial silvicultural treatments, riparian restoration treatments, juniper woodland treatments, aspen stand restoration and road restoration projects. LOCATION Recent Decisions - Lands Program 1 I I I I I Upper Spencer Creek Road Treatments - Road Upper Spencer Creek I' Implementation in July obliteration, decommissioning, realignment, improvement, T38S, R6E Sections Riparian Resenres DDRBs I 2M Mike Turaski and stream crossing removal. 15 and 23 12123103 Recent Decisions - Wildlife M Map 1 # 43 ecisions - Waters Map 1 # 21 Willow Valley Habitat Enhancement Willow Valley Warm water fishexies Implementation pending Reservoir ODFW involvement. Section 1 Exploration Quarry Expansion Drilling - Authorization for ODOT to conduct exploratory drilling in and around an existingpit to identify a source for additional mineral material. Scott Snedaker I I I I I I Recent Decisions - Fuels Treatment T40S, R6E, Sec. 1. N112NW114 Map 1 # 3 None Boundary Springs Yarding and Removal of Cut Juniper - Purpose of this project is to remove juniper boles in previously treated areas to reduce fuel accumulation and promote commercial use of juniper. None Ben Hall 1 & 2, Cerber Potholes, Sehnipps, and FIZ 95- 71 Juniper Yarding - to remove juniper boles in previously treated areas to reduce fuel accumulation and promote commercial use of juniper. Fint 360 acres yarded and material sold to Area FTZ- 1 04 utilization local mill ( REACH) that utilizes juniper. Exploration initiated as weather permits. Rebecca La& Linda Younger Mike Bechdolt Various Mike Bechdolt Klamath Falls Resource Area, Winter 2003 Planning Update - Page 3 Fuel treatment, juniper utilization DNA completed. Project on hold. BUREAU OF LAND MANAGEMENT KLAMATH FALLS RESOURCE AREA AVEl PHONE NUMBER: 2795 ANDERSON AVENUE, BLDG. # 25 ' E ( 541) 8836916 SPECIAL AREAS STATUS OF AEFECrED ANALYSIS PROJECT TITLE & DESCRIPTlON LOCATION AEFErnD COMPLETION DATE CONTACT r~ ann~ ng~ na~ ysis~ lrnp~ ernen- r Gareinoenr al RMP Evaluation~ Revision- In the final settlement agreement to the American Forest Resource Council vs. Bureau of Land Management ( BLM) litigation, the BLM is directed to revise Resource Management Plans ( RMPs) in western Oregon by December, 2008. The BLM began the revision process in 2003, evaluating current plans and developing a project preplan. Project status information will be posted on the District website. Formal scoping is expected in the second half of calendar year 2004. RMP Revision - FY 2008 None Resource Area Wide All Resources Evaluation in progress Don Homeins GerberlWillow Valley Coordinated Resource Management Plan ( CRMP) Watershed Analysis. - A local planning team of private landowners, StatelFederal land managers, and concerned citizens recommends future project implementation on private land in CRMP area. CRMP meetings/ discussions are continuing Map 1 # 5 GerberNillow Valley Watershed Completion date open-Rivate Lands ended Don Homeins Lany Frazier Wild and Scenic River designation, Area of Critical Concern, T& E spp. Map l # 28 Upper Klamath River Management Plan DEE - Develop a management plan in response to Wild and Scenic Riven Act requirements for river segment approx. 20 miles long encompassing 6,400 acres. Klarnath River - J. C. Boyle Reservoir, Oregon, to Copco One Reservoir, California Draft EIS released 511 612003. Comment period closed 8/ 13/ 2003. FEIS December 2004 Upper Klamath Basin and Wood River Wetland Resource Management Plan Amendment for the Fourmile Creek portion of this area. The purpose of this project is to amend the Upper Klamath Basin and Wood River Wetland RMP EIS to designate the Fourmile Creek area as an Area of Critical Environmental Concern. Riparian Wetland Area of Critical Environmental Concern ( ACEC) Draft EIS to be prepared. Specific schedule and completion date unknown. ACEC Evaluation submitted to District Manager, October 2000. Map 1 # 29 Fourmile Creek Wetland Lou Whiteaker Lany Frazier Draft MOU presented to the Tribal Council on 2/ 22/ 2000. Waiting for Tribal feedback. - -- Unknown Memorandum of Understanding ( MOU) between the Klamath Tribes and BLM for Coordination on Management Issues. - The proposed MOU identifies a process to coordinate tribal involvement with BLM management actions on public lands. Late- Successional Reserve ( LSR) Assessment. A single LSR Assessment was prepared to assess all 19 Unmapped LSRs designated within the resource area and develop management recommendations for these areas to restore or maintain late successional habitat. Former Tribal None Lakeview District Lands - None Draft submitted to and pending approval from the Regional Ecosystem Office ( REO). BLM lands west of Highway 97 covered by the Northwest Forest Plan Unmapped Late Successional - Reserves. Analysis is complete. - ou Whiteaker Klamath Falls Resource Area, Winter 2003 Planning Update - Page 4 2795 ANDERSON AVENUE, BLDG. # 25 KLAMATH FALLS, OR 97603 541) 8834916 STATUS OF COMPLETION DATE CONTACT AFFECTED I ANALYSIS I - Map 2 # 46 - None Map 1 -# 7 Map 1 # 22 - None Map 2 # 44 Map 2 # 30 Oak Thinning - Thin 100 acres of oak woodland to restore plant communities and reduce potential for stand replacing wildfires and overall fire management costs. Noxious Weed Treatments - contain1 reduce noxious weed populations using integrated pest management ( manual, mechanical, chemical, and biological control methods). Activities tier to KFRA Integrated Weed Control Plan ( IWCP) and EA- OR- 014- 93- 09 approved July 21, 1993. T40S, R6E, Sec. 35 T41S, R6E, Sec. 3 and 10 T41S, WE, Sec. 1 Weed- infested sites throughout the Klamath Falls Resource Area Bitterbrush Planting - - Various locations Ongoing Planning/ Analysisflmplementation - Vegetation Treatments I I I -- -- - Horton Rim I Windy Ridge Juniper Removal - Juniper treatment for fuel reduction and wildlife habitat inmovement GerberlWillow Valley Riparian Conifer Treatments - removing invasive juniper from riparian areas in the Gerber Block G& I Willow Valley Watersheds Spencer Creek Riparian Thinning- thin 80 acres of iuniverlmixed conifer T38S, R6E, Secs. 21 and 28 Clover Creek DDRB - 108 acres mechanical treatment. T. 38S, R6E, Sec. 27.34 Off Spencer Hookup Road I Document is tiered to the Northwest Area Noxious 1 Noxious Weed I Klamath River canyon/ ACEC None I Wyd Control Program Treatments occur May - EIS avvroved December I October on a vearlv I Lou mitaker Analysis in Progress. 1985: supplemented in March 1987. Analysis completion expected Spring 2004. - . basis. Mule deer winter range. Rob Roninger None I EA completed Riparian Reserves EA completed. I Ongoing - Possible in Key Watershed completion in 2004 I Mike Turaski cx completed. h j e c t in progress. Riparian, critical sucker habitat 2- 3 year implementation began Spring 2003. Ongoing Planning/ Analysis/ Implementation- Lands Treatments occur on a yearly basis. Hapa DNA completed. Bald Eagles, Survey and Manage species Map l # 8 Greg Reddell Map 1 # 17 Implementation initiated 2003 - Ongoing DNA completed in Spring 2001. Mike Turaski Map I -# 20 Map 1 -# 9 On hold for RE0 approval of LSRA - ~- - Dehlinger Trust - Residential Road ROW and easement. Bmner Land Exchange Steve Haper Bly Dump Sale ( EA No. OR- 014- 97- 01) - Purpose of # l8 this project is to sell Bly Transfer Station to Klamath Co. I of Bly'OrrgOn. Map I I None Known I Analysis in progress I Winter2004 Linda Younger T40S, RIOE, Sec. 9 South Bryant Mountain Al B ~ n eLra nd Sale Nancy Charley Trust Reciprocal Easement and ROW Klamath Falls Resource Area, Winter 2003 Planning Update - Page 5 None Unknown T41S, R13E. Sec. 14 T38S, RSE, Sec 12- 13 Reciprocal Easement Pending On hold Unknown Borders Riparian Reserve Winter 2004 Spring 2005 EA completedl Decision record pending CX completed, easement pending Linda Younger Linda Younger Spring 2004 Fall 2004 Linda Younger Linda Younger MAP PROJECT TITLE & DESCRIPTION REF. SPECIAL AREAS IC OMPLI AFFECTED Ongoing Planning/ Analysis/ Imp LOCATION ETION DATE I COMA dementation - rimber Sales I - - - Non - Non Roaming Salvage EA - The purpose is to provide NEPA coverage for timely salvage of timber mortality over the entire Resource Area. Entire Resource Area Unknown Preparing scoping letters. Spring 2004 I MI* cBechdo1t FY 04 - Baldy Salvage Timber Sale - Sale is designed to harvest windthrown trees as a result of 2003- 4 windstorms and scattered insect and disease related mortality. Anticipated volume is I . O- 1 SMMBF on 300- 500 acres. FY 04 - Matchbox Title I1 Service Contradl'imber Sale - The project consists of a Forest Health Density ManagementIUnderstory Thinning of overstocked mixed conifer stands. The sale is being designed under the Secure Rural Schools and Community Self- Determination Act of 200 - Public Law 106- 393. A service contract will be used to thin, yard, and deck trees from an overstocked mixed conifer stand. A timber sale contract will be used sell the decked material. Approximately 300 acres are scheduled for treatment resulting in about 600 MBF. Primarily in the Surveyor Mtn and Burton Butte Areas. May also include some eastside areas. Timber Sale is scheduled to be sold in Mike Bechdolt May or June of 2004 Presently marking some of the scatted salvage Matrix Contract is scheduled to be awarded in June or Mike Bechdolt July of 2004 Chase Mountain Area T. 40S., R. 7E., Sec. 9 Presently Preparing the Matrix Timber Sale Contract Proposed sale date: Summer 2005 Mike Bechdolt Riparian Reserves T38S., ME., Sec. l3,15,23, 25 and 26 Reserves! Matrix Buck Again Timber Sale - An estimated 700 acres is designed for treatment in the Spencer Creek watershed near Buck Lake. Approx. 4 MMBF to be harvested. Sale preparation. Chew Timber Sale- Approximately 1,000 acres density management understory reduction adjacent to and south of T40S. R6E, Secs. 1, 1 1,14 T40S, R7E. Secs. 3 and 5 Proposed sale date Mike Bechdolt Hwy 66 west of la math Falls. ~ aleanal~ zuendd er the Sale preparation. Spring 2004 or 2005. Topsy/ Pokegama/ Hamaker EA (# OR- 0 14- 98- 01 ). Estimated volume of 2.5 m b f . None Oneoine Plannine/ Analvsis/ Implementation - Roads and Facilities Map 1 # 77 Map # 73 Klamath Falls Resource Area, Winter 2003 Planning Update - Page 6 Sediment Traps - 30 sediment traps on BLM, USFS, and private land Map I # 6 Gcrber Road Sediment Reduction - road resurfacing and drainage improvement to reduce sediment delivery to streams in the Gerber Watershed Spencer Creek Watershed and Gerber Block Gerber Washrack- Installation of facility at Gerber Guard Station for washing equipment to control the suread of noxious weeds and overhead filling of tankers. 5 stream crossings None Gerber Guard Station Critical sucker habitat DNA completed. Sediment traps installed. Noxious weed prevention EA completed. Implementation initiated I Fall 2004 Monitoring in progress. Mike Turaski CX completed. Mike Turaski Pending funding. Bob Crumrine/ Brian McCarty - I - 1 - Map 1 # 6 Ongoing Planning/ Analysis/ Implementation - Roads and Facilities ( continued) Gerber Area Recreation Improvements - ( RMP ROD EIS 6- 2- 95, pp. 49- 50) - Project falls under corrective maintenance, improvement or replacement in the Klamath Falls RMP. Existing maintenance, improvement or replacement include: rocking and chip- sealinglpaving road system and campsites, picnic tables, barrier posts, camp host RV holding tank, hydrants, Barnes Valley Boat Ramp access road. Scott Smter Gerber Reservoir Recreation Site Gerber Area Primitive Camp and Day Use Sites Recreation Improvements. The objectives of these improvements are to update or improve existing facilities to continue to provide an enhanced recreational experience and satisfy visitor needs. T& ESpecies ( suckers and bald eagles) Scott Senter Stan H Spring, Potholes, Miller Creek, Frog Camp, Pitchlog Creek, Wildhorse, Basin, Rock Creek and Willow Valley Reservoir Map l # 6 Projects in compliance GththeKFIURMP. Determination of NEPA Adequacy completed and approved on 10128199. Wood River Wetlands Project - Remaining projects: Finish installation of fish screen on 7- mile Canal diversion structure and floating boardwalk, interpretive signs, and trail system. Surface rock dike roads from bridge to 7- mile Canal and add group interpretive site. Juniper Chip Road - Using juniper debris for biomass or by- product in Oshea ( mZ 95/ 71), and Norcross Springs. FY 2004 - Miller Creek- Potholes trail to be constructed T& E Species ( suckers) wood River Property I I Upper Klamath Basin and Wood River Wetland I A Determination of NEPA Adequacy ( DNA) completed 9/ 25/ 2000. ( Project contingent on funding) Map 1 # 25 - Map 2 # 70 FY 2004- sidewalks and pinic tables to be installed at Willow Valley Res. Wedge Watkins Joe Foran 25 miles north of Klamath Falls, Oregon T 39 8 40s. R13,14,14XE I None Known I I Stewardship contract EAcompIeted being developed. Ongoing Projects - Prescribed Burning and Fuels Treatment Wetlands Map 2 # 2 Resource Management Plan EIS; decision signed June 16,1995. Joe Foran Pending funding Short Lake Broadcast Bum - Prescribe bum approx. 280 acres outside FTZ to reduce fuel loading and risk of wildfire. T38S. R1 I E, Sec 20 & 29 - - - - - - -- - - - - - Miller Creek Mechanical Treatment - Proposal to use mechanical piling instead of prescribed buming of a~ oroximatelv I00 acres. Map 2 # 37 - T39S. R13E. Sec. 14 & 23 Analysis Completed ACEC 1 FONSl and Decision Record on 3- 24- 99. Joe Foran None Known Project delayed. EA completed Fuels Maintenance Treatments # t ( KCER - 00- 03) Treat approximately 1,200 acres to remove fire- prone brush, excessive levels of hazardous fuels ( less than 6" in diameter), and small conifers that are ladder fuels and threats to over stow trees bv crown fire.. Map 2 # I 1 Spring 2004 Klamath Falls Resource Area, east of Hwy 97. See Prescribed Fire Map for locations. None Known Dale Brush Map 2 # 62 Analysis completed. Multiple year implementation - ongoing. Mechanical Slash Treatment Project - Mechanical treatments ( shearing, chipping, or grinding) to reduce fuels and control vegetation on approx. 12,000 acres. Joe Foran Multiple Locations Resource Area Wide None / Second DNA completed. Klamath Falls Resource Area, Winter 2003 Planning Update - Page 7 Projects tasked out over a three year period - ongoing. PROJECT K. 1 TITLE & DESCRIPTIO SPECIAL AREAS STATUS OF 4 CONTACT AFFECTED ANALYSIS - Map 2 -# 39 Map 2 # 40 - Map 2 -# 42 Map 2 # 38 Map 2 # 63 Map 2 # 64 - Map 2 # 65 & # I9 Map 2 # 45 - Map 2 # 49 - Stukel98- 1 Mechanical Treatment - Mechanical piling T40S, RIOE, Sec. 10,11,14, instead of pmcribed burning of approximately 500 acres. 23,24 Stukel98- 2 Prescribed Burn - Prescribe bum approx. 3,000 acres to: Reintroduce fire to restore plant communities, while reducing the potential for stand-replacement wildfires and overall fire management costs. T40S, RIOE, Sec. 12,13,24 T40S, RllE, Sec. 7& 18 HamakerIChase Fuels Treatment - Reduce Fuels on T40S, R8E 4000 acres south of Hwy 66 I Stiles Spring Prescribed Burn - Project purpose to bum approximately 1,000 acres to: Reinduce fire to restore sustainable function and structure to plant communities, while reducing the potential for stand- replacement wildfires, and reducing overall fire management costs. Stukel98- 7 & 9 Prescribed Burns - Prescribe bum approximately 525 acres to: reintroduce fire to restore plant communities, reduce overall fire management costs and the potential for stand- replacing wildfires. Statelinel Holbmk Prescribed Bums - Presmie bum approximately 4.000 acres to reduce fuel loading and risk of catastrophic wildfire. T37S, RIOE, Sec. 3- 5,9- 11, 14- 15 T40S, RllE, Sec5 & 6 T. 40S, R15 E., T. 41S, RISE. -- Big Adobe Prescribed Burn - Prescribe bum approximately 6,700 acres to reduce fuel loading and risk of catastrophic wildfire ( includes Wild Midway Rx Bum) Range- Juniper Treatment - Hazardous fuel reduction, T40S. R12E. Sec. 1 1 using mechanical and prescribed fire methods. T41 S, RISE Upper Swan Prescribed Burn - Project purpose: bum approximately 98 acres to restore sustainable function and structure to plant communities, reduce potential for stand-replacement wildfires and overall fire management costs. g and Fuels Treatment ( continued) None Known Project0 t1ie 4r- s9 4to- 0E9A. # OR- Project ongoing Joe Fmn T37S, RIOE, Sec. 24 & 25 T37S, RI 1.5E, Sec. 31 Bald Eagle ( Analysis Completed- I 200 acres treated in FY I None Analysis Completed Project tiers to EA # OR- 014- 94- 09. EA completed Wildlife Habitat Riparian Initiated Winter 2001 Fall 2004 Joe Foran Project delayed until the Spring 2004 Bald None Bald Eagle I Planned projects tier to the Promammatic Fire I Joe Foran Joe Foran Project initiated, 2- 3 year implementation FONSI - 12- 1 9- 99. 2000; Remainder Decision Record on 01 - 25- 2000 ,, Foran Joe Foran Analysis Completed Project tiers to EA # OR- 014- 94- 09) approved on 4- 29- 94. Initiated Winter 2001 Klamath Falls Resource Area, Winter 2003 Planning Update - Page 8 Wildlife forage/ habitat improvement 130 acres completed Remainder Spring 2004 Accomplished 1500 acres. Remainder Fall 2004. Steve Pehick- Underwood Joe Foran DNA completed ongoing 2- 3 year implementation Joe Foran .. " "" . 7 < .,.. - . . 7 - " b - . " < * - - ' 7 , 4 . , v ,-' w., ,. ' q"* -?, . x-.. s,... >,% VW? P ,.- 7i,- .. x., < 8 SCHEDULE OF PROPOSED PROJECTS BUREAU OF LAND MANAGEMENT KLAMATH FALLS RESOURCE AREA 2795 ANDERSON AVENUE, BLDG. # 25 KLAMATH FALLS, OR 97603 PHONE NUMBER: ( 541) 883- 69 MAP PROJECT TITLE & DESCRIPTION LOCATION I SPECIAL AREAS STATUS OF ANALYSIS COMPLETION CONTACT REF. # AFFECTED DATE Rangeland Health Standards Assessments - in progress I These assessments compare the monitoring information collected against the five Standards for Rangeland Health and propose management changes if current grazing use is not meeting the Standards, or not making significant improvement towards meeting them. Changes are implemented through the grazing decision or agreement process. z3I Re16 Allotment ( M893) I South Langell Valley I None Known I Assessment in progress I Summer 2004 I Dana Eckard M$\ 3 I KIamatL Forest Estates Allotment ( M862) 1 North of Bonanza -~ Yainax Allotment ( M861) I None Known I Assessment in progress I ~ ~ - 2 0 0 4 I Bill Lindsey North of Bonanza Map # 55 None Known ? G3 Haskins Allotment (# 0826) y&' Assessment in progress Masten Allotment ( M842) Map # 68 North of Bonanza Kellian Allotment (# 0834) Hungry Hollow Allotment (# 0830) Klamath Falls Resource Area, Winter 2003 Planning Update - Page 9 SUM 2004 North of Bonanza Adams Allotment (# 0800) Rangeland Health Standards Assessments - completed* Bill Lindsey None Known North of Bonanza North of Bonanza None Known East of Bonanza Bill Lindsey Assessment in progress None Known None Known * A total of 37 Rangeland Health Standards Assessments have been completed to date, 1 has been completed so far in FY 2004. Assessment in progress None Known None Known Assessment completed Summer 2004 Assessment in progress Assessment in progress Map North of Bonanza December 2003 # 48 Dana Eckard Summer 2004 Assessment in progress McCartie Allotment (# 0860) Dana Eckard Summer 2004 Summer 2004 Dana Eckard Summer 2004 Dana Eckard Dana Eckard Presentations/ Environmental Education Programs/ Tours ( Fiscal Year to Date) Fun With Fungi I 1 1/ 2/ 03 I Seven Mile Area Adults 25 I What Was Presented Overview of past and current outreach events; permit sales Wood River Wetland Field Trip Operation Indian Rocks ARPA Investigation 1 1 1/ 3/ 03 ( Central Washington University 1 Faculty and Students I 51 I Date 1 Group / Age # of People 1 01 1 5/ 03 10/ 28/ 03 Where Cultural Resource Management and the NEPA Process Archaeological Investigations in the Great Basin I Wildlife Management 1 12/ 16/ 03 1 OIT - " Expanding Horizons" I 8* Grade Students I 120 1 Ross Ragland Theater Wood River Wetland Coloring Books 1 1/ 3/ 03 1 1/ 4/ 03 Klarnath Falls Resource Area, Winter 2003 Planning Update - Page 10 Answer People/ Adults Oregon Institute of Technology Students I 1 1 11 9/ 03 Shasta Elementary School -- - S - 290 Fire Behavior 25 - 30 Central Washington University Central Washington University Elementary Students 30 12/ 20/ 03 Graduate Student Seminar Graduate Student Seminar 24 35 Klamth Community College Adults 8 EventIActivlty Date Location Contact( s) F 01 rarnclpanrs ( EmployeeslPublic) IBald Eagle Conference I Februaryl3- IS I Oregon Institute of Technology I Steve Haynerl Kelly Hollums I l~ arthD ay I April I Jefferson Square Mall I Greg Reddell I Klamath Watershed conference February 24 - 26 Wilderness & Horse Packing Clinic* International Migratory Bird Day IMBD Pre- event Classes -- - IMBD Educator Workshop Oregon Institute of Technology May ( IMBD) April 24 IMBD Event National Free Fishing Day RAP Camp Klamath County Fair Klamath Falls Resource Area, Winter 2003 Planning Update - Page 11 Wedge WatkinslKelly Hollums April 16 - pp - - Sixth Grade Forestry Tour National Public Lands Day Oregon Archeology Celebration Klarnath County Fairgrounds Klamath Community College May 8 June June August Tonya PinckneyIScott Senter Steve Hayner, et al OSU- Klamath Co. Extension * Numbers of public participants for large events are estimated. ** BOLD WRITING indicates that project is funded with District Outreach dollars. September September September Veteran's Park To Be Announced Camp Esther Applegate Klamath County Fairgrounds Steve Hayner, et al Steve Hayner Scott Snedaker To Be Announced PinckneylSenter Clover Creek Educational Area To Be Announced To Be Announced ~ p Bill Johnson To Be Announced Michelle Durant Glama th Falls Resource Area Miscellaneo~ wP roject Loca ticms R6E RBE R7E RBE RBE RlOE RIIE R12E R13E R14E R14.6E R16E Klamath Falls Resource Area, Winter 2003 Planning Update - Page 12 N LEGEND R5E R6E R7E R8E RQE RIOE R l l E R12E R13E R14E R14.5E R15E Klarnath Falls Resource Area, Fall 2003 Planning Update - Page 13 UNITED STATES DEPARTMENT OF THE INTERIOR BUREAU OF LAND MANAGE~ ENT Klarnath Falls Resource Area Office 2395 Parderson Avenue, Building a 5 Kfamth MIS. Oregan 97603 OF. FIGIAL, BUSI~ ESS PENALTY FOR PRIVATE USE, $ 300 Marita Kunkel Library Director Oregon Institute of Techolagy 3201 Cempus Dr Klamath Falls, OR 97601

1592. [Image] Relation between selected water-quality variables and lake level in Upper Klamath and Agency Lakes, Oregon


	Relation Between Selected Water-Quality Constituents and Lake Stage in Upper Klamath and Agency Lakes, Oregon By Tamara M. Wood, Gregory J. Fuhrer, and Jennifer L. Morace SUMMARY Upper Klamath Lake is ...
	Citation Citation Citation Abstract Copy Title: Relation between selected water-quality variables and lake level in Upper Klamath and Agency Lakes, Oregon Author: Wood, Tamara M. Year: 1996, 2005, 2004 Relation Between Selected Water-Quality Constituents and Lake Stage in Upper Klamath and Agency Lakes, Oregon By Tamara M. Wood, Gregory J. Fuhrer, and Jennifer L. Morace SUMMARY Upper Klamath Lake is a large (140 square-mile), shallow (mean depth about 8 ft) lake in south-central Oregon that the historical record indicates has been eutrophic since its discovery by non-Native Americans. In recent decades, however, the lake has had annual occurrences of near-monoculture blooms of the blue-green alga Aphanizomenon flos-aquae. In 1988 two sucker species endemic to the lake, the Lost River sucker (Deltistes luxatus) and the shortnose sucker (Chasmistes brevirostris), were listed as endangered by the U.S. Fish and Wildlife Service, and it has been proposed that the poor water quality conditions associated with extremely long and productive blooms are contributing to the decline of those species. It has also been proposed that the low lake levels made possible by the construction of a dam at the outlet from the lake in 1921 have contributed to worsening water quality through a variety of possible mechanisms (Jacob Kann, Klamath Tribes, written com-mun., 1995). One such mechanism would be an increase in internal phosphorus loading from resuspended sediments (Jacoby and others, 1982), resulting from an increase in bottom shear stresses at lower lake levels (Laenen and LeTourneau, 1996), leading in turn to more intense algal blooms. Another possible mechanism is an earlier triggering of algal blooms. When early spring lake levels are low, greater light intensity at the sediment surface might speed recruitment of algal cells from the sediments. Sediment recruitment has been shown to be an important contributor to water column biomass increases in A. flos aquae (Barbiero and Kann, 1994) and Gloeotrichia echinulata (Barbiero, 1993). An earlier bloom could result in poor water quality conditions occurring earlier in the year, when young-of-the-year fish may be more susceptible to those conditions. Lake level can also influence water quality directly. An increased frequency of sediment resuspension at lower lake levels could increase chemical and biological oxygen demand, resulting in decreased dissolved oxygen concentrations. Sediment oxygen demand also may be enhanced at lower lake levels because it is concentrated over a smaller volume of water. Some compensation for increased oxygen demand at lower lake levels might be provided by increased reaeration, if the water column mixes from top to bottom more frequently. Based on the analysis of data that they have been collecting for several years, the Klamath Tribes recently recommended that the Bureau of Reclamation (Reclamation) modify the operating plan for the dam to make the minimum lake levels for the June-August period more closely resemble pre-dam conditions (Jacob Kann, written commun., 1995). The U.S. Geological Survey (USGS) was asked to analyze the available data for the lake and to assess whether the evidence exists to conclude that year-to-year differences in certain lake water-quality variables are related to year-to-year differences in lake level. The results of the analysis will be used as scientific input in the process of developing an operating plan for the Link River Dam. Datasets Two water-quality datasets were analyzed. The first was a series of hourly records of pH, dissolved oxygen, and water temperature, each of approximately a week's duration. The records were collected at 3 sites over 3 years, 1992 through 1994, with enough consistency to define the seasonal patterns. This dataset provided information about the diel extremes in dissolved oxygen and pH and the seasonal pattern in the diel cycle, but measurements were limited to a depth of 1 m(3.28 ft). The second dataset was a set of depth profiles of pH and dissolved oxygen and concurrent depth-integrated samples for nutrients and chlo-rophyll-a. The profiles were collected at approximately biweekly intervals at nine sites (seven in Upper Klamath and two in Agency Lake) over the 5 years 1990 through 1994. These depth profiles provided information on the depth-dependence of dissolved oxygen and pH, and allowed more extensive year-to-year comparisons than did the hourly records. Because measurements were made at each site only once during the sampling day, however, they did not capture the daily extremes in water quality. Lake level is measured daily by the USGS at three sites around the lake: Rocky Point, Rattlesnake Point, and near the city of Klamath Falls. These daily measurements are then used to compute a spatially weighted average of the lake level that is reported in the USGS annual Water-Data Report for Oregon. The average lake levels were used in this report. Two climatic datasets were used in this report; both were collected at the Klamath Falls airport. Air temperature was recorded as a daily maximum and daily minimum value. Cloud cover was quantized on a daily basis into one of seven levels. Because the focus of this study was primarily to examine possible relations between water quality and lake level, the lake level data provide an important context for the discussions that follow. Title: Relation between selected water-quality variables and lake level in Upper Klamath and Agency Lakes, Oregon Author: Wood, Tamara M. Year: 1996, 2005, 2004 Relation Between Selected Water-Quality Constituents and Lake Stage in Upper Klamath and Agency Lakes, Oregon By Tamara M. Wood, Gregory J. Fuhrer, and Jennifer L. Morace SUMMARY Upper Klamath Lake is a large (140 square-mile), shallow (mean depth about 8 ft) lake in south-central Oregon that the historical record indicates has been eutrophic since its discovery by non-Native Americans. In recent decades, however, the lake has had annual occurrences of near-monoculture blooms of the blue-green alga Aphanizomenon flos-aquae. In 1988 two sucker species endemic to the lake, the Lost River sucker (Deltistes luxatus) and the shortnose sucker (Chasmistes brevirostris), were listed as endangered by the U.S. Fish and Wildlife Service, and it has been proposed that the poor water quality conditions associated with extremely long and productive blooms are contributing to the decline of those species. It has also been proposed that the low lake levels made possible by the construction of a dam at the outlet from the lake in 1921 have contributed to worsening water quality through a variety of possible mechanisms (Jacob Kann, Klamath Tribes, written com-mun., 1995). One such mechanism would be an increase in internal phosphorus loading from resuspended sediments (Jacoby and others, 1982), resulting from an increase in bottom shear stresses at lower lake levels (Laenen and LeTourneau, 1996), leading in turn to more intense algal blooms. Another possible mechanism is an earlier triggering of algal blooms. When early spring lake levels are low, greater light intensity at the sediment surface might speed recruitment of algal cells from the sediments. Sediment recruitment has been shown to be an important contributor to water column biomass increases in A. flos aquae (Barbiero and Kann, 1994) and Gloeotrichia echinulata (Barbiero, 1993). An earlier bloom could result in poor water quality conditions occurring earlier in the year, when young-of-the-year fish may be more susceptible to those conditions. Lake level can also influence water quality directly. An increased frequency of sediment resuspension at lower lake levels could increase chemical and biological oxygen demand, resulting in decreased dissolved oxygen concentrations. Sediment oxygen demand also may be enhanced at lower lake levels because it is concentrated over a smaller volume of water. Some compensation for increased oxygen demand at lower lake levels might be provided by increased reaeration, if the water column mixes from top to bottom more frequently. Based on the analysis of data that they have been collecting for several years, the Klamath Tribes recently recommended that the Bureau of Reclamation (Reclamation) modify the operating plan for the dam to make the minimum lake levels for the June-August period more closely resemble pre-dam conditions (Jacob Kann, written commun., 1995). The U.S. Geological Survey (USGS) was asked to analyze the available data for the lake and to assess whether the evidence exists to conclude that year-to-year differences in certain lake water-quality variables are related to year-to-year differences in lake level. The results of the analysis will be used as scientific input in the process of developing an operating plan for the Link River Dam. Datasets Two water-quality datasets were analyzed. The first was a series of hourly records of pH, dissolved oxygen, and water temperature, each of approximately a week's duration. The records were collected at 3 sites over 3 years, 1992 through 1994, with enough consistency to define the seasonal patterns. This dataset provided information about the diel extremes in dissolved oxygen and pH and the seasonal pattern in the diel cycle, but measurements were limited to a depth of 1 m(3.28 ft). The second dataset was a set of depth profiles of pH and dissolved oxygen and concurrent depth-integrated samples for nutrients and chlo-rophyll-a. The profiles were collected at approximately biweekly intervals at nine sites (seven in Upper Klamath and two in Agency Lake) over the 5 years 1990 through 1994. These depth profiles provided information on the depth-dependence of dissolved oxygen and pH, and allowed more extensive year-to-year comparisons than did the hourly records. Because measurements were made at each site only once during the sampling day, however, they did not capture the daily extremes in water quality. Lake level is measured daily by the USGS at three sites around the lake: Rocky Point, Rattlesnake Point, and near the city of Klamath Falls. These daily measurements are then used to compute a spatially weighted average of the lake level that is reported in the USGS annual Water-Data Report for Oregon. The average lake levels were used in this report. Two climatic datasets were used in this report; both were collected at the Klamath Falls airport. Air temperature was recorded as a daily maximum and daily minimum value. Cloud cover was quantized on a daily basis into one of seven levels. Because the focus of this study was primarily to examine possible relations between water quality and lake level, the lake level data provide an important context for the discussions that follow.

1593. [Image] Chronic toxicity of low dissolved oxygen concentrations, elevated pH, and elevated ammonia concentrations to lost river suckers (deltistes luxatus), and swimming performance of lost river suckers at various temperatures.


	The study examines two species of sucker,the shortnose sucker(chasmistes brevirostrix), and the Lost River sucker,(deltisties luxatus) that inhabit Upper Klamath Lake and the effects of chronic toxicity ...
	Citation Citation Citation Abstract Copy Title: Chronic toxicity of low dissolved oxygen concentrations, elevated pH, and elevated ammonia concentrations to lost river suckers (deltistes luxatus), and swimming performance of lost river suckers at various temperatures. Author: Meyer, Joseph S. Year: 2000, 2007, 2006 The study examines two species of sucker,the shortnose sucker(chasmistes brevirostrix), and the Lost River sucker,(deltisties luxatus) that inhabit Upper Klamath Lake and the effects of chronic toxicity and temperature changes. The study examines two species of sucker,the shortnose sucker(chasmistes brevirostrix), and the Lost River sucker,(deltisties luxatus) that inhabit Upper Klamath Lake and the effects of chronic toxicity and temperature changes. Title: Chronic toxicity of low dissolved oxygen concentrations, elevated pH, and elevated ammonia concentrations to lost river suckers (deltistes luxatus), and swimming performance of lost river suckers at various temperatures. Author: Meyer, Joseph S. Year: 2000, 2007, 2006 The study examines two species of sucker,the shortnose sucker(chasmistes brevirostrix), and the Lost River sucker,(deltisties luxatus) that inhabit Upper Klamath Lake and the effects of chronic toxicity and temperature changes. The study examines two species of sucker,the shortnose sucker(chasmistes brevirostrix), and the Lost River sucker,(deltisties luxatus) that inhabit Upper Klamath Lake and the effects of chronic toxicity and temperature changes.

1594. [Image] The Endangered Species Act and its impact on agricultural producers: hearing before the Subcommittee on Conservation, Credit, Rural Development, and Research of the Committee on Agriculture, House of representatives, One Hundred Eighth Congress, second session, July 26, 2004, Greely, CO.


	CONTENTS Lucas, Hon. Frank, a Representative in Congress from the State of Oklahoma, opening statement .................................................................................... 1 Musgrave, ...
	Citation Citation Citation Abstract Copy Title: The Endangered Species Act and its impact on agricultural producers: hearing before the Subcommittee on Conservation, Credit, Rural Development, and Research of the Committee on Agriculture, House of representatives, One Hundred Eighth Congress, second session, July 26, 2004, Greely, CO. Author: United States. Congress. House. Committee on Agriculture. Subcommittee on Conservation, Credit, Rural Development, and Research. Year: 2004, 2005 CONTENTS Lucas, Hon. Frank, a Representative in Congress from the State of Oklahoma, opening statement .................................................................................... 1 Musgrave, Hon. Marilyn N., a Representative in Congress from the State of Colorado, opening statement........................................................................... 2 Witnesses Foutz, Alan, president, Colorado Farm Bureau, Centennial, CO ........................ 10 Prepared statement .......................................................................................... 38 George, Russell, executive director, Colorado Department of Natural Resources, Denver, CO............................................................................................. 4 Prepared statement .......................................................................................... 29 Palmer, William, executive director, Rocky Mountain Bird Observatory, Brighton, CO ........................................................................................................ 16 Prepared statement.......................................................................................... 60 Sims, James T., executive director, Western Business Roundtable, Golden, CO.......................................................................................................................... 13 Prepared statement .......................................................................................... 43 Stetson, Jean, co-chairman, Endangered Species Committee, Colorado Cattlemen, Craig, CO..................................................................................................... 7 Prepared statement .......................................................................................... 36 Submitted Material Weege, Merle, secretary, Ginseng Board of Wisconsin, statement...................... 65 Title: The Endangered Species Act and its impact on agricultural producers: hearing before the Subcommittee on Conservation, Credit, Rural Development, and Research of the Committee on Agriculture, House of representatives, One Hundred Eighth Congress, second session, July 26, 2004, Greely, CO. Author: United States. Congress. House. Committee on Agriculture. Subcommittee on Conservation, Credit, Rural Development, and Research. Year: 2004, 2005 CONTENTS Lucas, Hon. Frank, a Representative in Congress from the State of Oklahoma, opening statement .................................................................................... 1 Musgrave, Hon. Marilyn N., a Representative in Congress from the State of Colorado, opening statement........................................................................... 2 Witnesses Foutz, Alan, president, Colorado Farm Bureau, Centennial, CO ........................ 10 Prepared statement .......................................................................................... 38 George, Russell, executive director, Colorado Department of Natural Resources, Denver, CO............................................................................................. 4 Prepared statement .......................................................................................... 29 Palmer, William, executive director, Rocky Mountain Bird Observatory, Brighton, CO ........................................................................................................ 16 Prepared statement.......................................................................................... 60 Sims, James T., executive director, Western Business Roundtable, Golden, CO.......................................................................................................................... 13 Prepared statement .......................................................................................... 43 Stetson, Jean, co-chairman, Endangered Species Committee, Colorado Cattlemen, Craig, CO..................................................................................................... 7 Prepared statement .......................................................................................... 36 Submitted Material Weege, Merle, secretary, Ginseng Board of Wisconsin, statement...................... 65

1595. [Image] Monitoring of Lost River and Shortnose suckers and shoreline spawning areas in Upper Klamath Lake, 1999


	Monitoring of Lost River and Shortnose Suckers at Shoreline Spawning Areas in Upper Klamath Lake, 1999 Prepared by: Rip S. Shively1 Mark F. Bautista2 Andre E. Kohler2 1 U. S. Geological Survey, Biological ...
	Citation Citation Citation Abstract Copy Title: Monitoring of Lost River and Shortnose suckers and shoreline spawning areas in Upper Klamath Lake, 1999 Author: Shively, Rip S.; Bautista, Mark F.; Kohler, Andre E. Year: 1999, 2005 Monitoring of Lost River and Shortnose Suckers at Shoreline Spawning Areas in Upper Klamath Lake, 1999 Prepared by: Rip S. Shively1 Mark F. Bautista2 Andre E. Kohler2 1 U. S. Geological Survey, Biological Resources Division Klamath Falls Duty Station 6937 Washburn Way Klamath Falls, OR 97603 2 Johnson Controls World Services Inc. NERC Operation Post Office Box 270308 Fort Collins, CO 80527 Executive Summary In 1999, we sampled Lost River { Deltistes luxatus) and shortnose ( Chasmistes brevirostris) suckers from 5 April to 17 June at five shoreline spawning locations in Upper Klamath Lake ( UKL). Trammel nets were set to encompass identified spawning areas and were fished approximately 1- 1.5 hours before sunset until 3 hours after sunset or until 20 or more fish were captured. A total of 808 Lost River and 19 shortnose suckers were captured from Sucker, Silver Building, Ouxy, and Boulder springs, and Cinder Flats. The majority of Lost River suckers were captured at Cinder Flats ( 35%) and Sucker Springs ( 34%), followed by Ouxy Springs ( 16%), Silver Building Springs ( 12%), and Boulder Springs ( 3%). Males dominated the catch at all sites, but the sex ratios at Cinder Flats and Silver Building Springs were particularly skewed towards males. We recaptured 32 Lost River suckers that had been tagged during previous years sampling efforts. All of these fish, with the exception of two fish tagged at Ball Point in July, were originally tagged during the spawning season at shoreline spawning areas in UKL. This information provides further evidence that distinct stocks of Lost River suckers exist based on spawning location ( i. e., UKL and Williamson River). We also recaptured 23 Lost River suckers that were tagged in 1999 at shoreline spawning areas. Approximately half of these fish were recaptured at different locations than tagged indicating these fish were moving between spawning areas. The size offish captured at shoreline spawning areas decreased as the spawning season progressed, although the decrease in size was not as dramatic as reported in previous years. A limited number of shortnose suckers were captured at shoreline spawning areas in 1999, with a majority sampled after 1 May. Previous data for shortnose suckers at these sites is limited with respect to size, timing of spawning, sex composition, and relative numbers. Continuation of systematic sampling efforts at shoreline spawning areas will provide valuable information on the demographics and life history of Lost River and shortnose suckers utilizing these areas. Acknowledgements We thank Anita Baker, Brooke Bechen, Lani Hickey, and Tonya Wiley for assisting with sampling offish at shoreline spawning areas. Mark Buettner and Brian Peck ( U. S. Bureau of Reclamation) provided support during the early phases of our sampling as well as helpful comments on this report. We also appreciate the cooperation and support of Larry Dunsmoor ( Klamath Tribes) for identifying spawning areas, providing logistical support, and for the thoughtful review of this report. Cassandra Watson and Elizabeth Neuman produced finalized versions of tables and figures within this report and their efforts are greatly appreciated. This research was funded by the U. S. Geological Survey, Biological Resources Division through the Western Reservoirs Initiative. Introduction Severe water quality problems in Upper Klamath Lake ( UKL) have led to critical fisheries concerns for the region. Historically, UKL was eutrophic but has become hypereutrophic ( Goldman and Home 1983) presumably due to land- use practices within the basin ( USFWS 1993). As a result, the algal community has shifted to a monoculture of the blue- green algae Aphanizomemon flos- aquae and massive blooms of this species have been directly related to poor water quality episodes in UKL. The growth and decomposition of dense algal blooms in the lake frequently cause extreme water quality conditions characterized by high pH ( 9- 10.5), widely variable dissolved oxygen ( anoxic to supersaturated), and high ammonia concentrations (> 0.5 mg/ 1 unionized). In addition to water quality problems associated with A. flos- aquae, it is believed the loss of marsh habitat near the lake, timber harvest, removal of riparian vegetation, livestock grazing, and agricultural practices within the basin has contributed to hypereutrophic conditions. It is likely that these disturbances have altered the UKL ecosystem substantially enough to contribute to the near monoculture of A. flos- aquae. Investigations in 1913 documented the algal community as a diverse mix of blue- green and diatom communities, however, by the 1950' s A. flos- aquae was dominant ( USFWS 1993). The Lost River sucker ( Deltistes luxatus) and shortnose sucker ( Chasmistes brevirostris) are endemic to the Upper Klamath Basin of California and Oregon ( Moyle 1976). Declining population trends for both species were noted as early as the mid- 1960' s, however, the severities of the population declines were not evident until the mid- 1980' s. In 1988 the U. S. Fish and Wildlife Service listed both Lost River and shortnose suckers as endangered. Suspected reasons for their decline included damming of rivers, dredging and draining of marshes, water diversions, hybridization, competition and predation by exotic species, insularization of habitat, and water quality problems associated with timber harvest, removal of riparian vegetation, livestock grazing, and agricultural practices ( USFWS 1993). The U. S. Geological Survey, Biological Resources Division ( BRD) has been conducting field investigations on Lost River and shortnose suckers in UKL since 1994. The majority of these sampling efforts have focused on catching fish in UKL and the Lower Williamson River. Sampling in the Lower Williamson River focused on developing indices of relative abundance of Lost River and shortnose suckers. In 1999, Oregon State University continued sampling in the Lower Williamson River fishing trammel nets from April to August at four standardized locations. In addition to sampling efforts in the Lower Williamson River, BRD crews conducted periodic sampling at several shoreline spawning areas on the east side of UKL. This sampling was beneficial because it provided information on species composition, size, and sex ratios of suckers utilizing these areas. However, temporal changes in abundance may have been missed because consistent sampling never occurred throughout the entire spawning season ( Perkins et al, In preparation). Recently, there has been increased concern on the effects of water level management in UKL on spawning suckers. Information is needed on the timing, relative abundance, and distribution of sucker spawning in UKL to make informed decisions with respect to management of lake elevation. In 1999, we conducted systematic trammel netting surveys at Sucker, Silver Building, Ouxy, and Boulder springs and Cinder Flats along the east shore of UKL. In addition, we sampled periodically at Barkley Springs and Modoc Point to determine if suckers were utilizing these areas for spawning. This report summarizes data collected in 1999 on shoreline spawning populations of Lost River and shortnose suckers with emphasis on timing, species composition, sex ratios, and relative abundance. Methods We conducted systematic trammel netting surveys at five locations along the east shore of UKL ( Figure 1). We began sampling at Cinder Flats, Sucker, Silver Building, and Ouxy springs in early April with Boulder Springs added to the list of sampling sites on 27 April. In addition to these sites, we periodically sampled at Barkley Springs and Modoc Point ( Table 1). We attempted to sample each site twice per week although certain sites were only sampled once per week when catch rates of suckers were low ( i. e., less than 5 fish per evening). Trammel nets were fished for about 4 hours ( approximately 1- 1.5 hours before sunset until 3 hours after dark) or until we captured 20 or more fish. Nets used at individual sites varied in length from 15- 30 m, were 1.8 m tall with two outer panels ( 30cm bar mesh), an inner panel ( 3.8 cm bar mesh), a foam core float line, and a lead core bottom line. Generally, we set 1- 2 nets starting at the shoreline and extending out to encompass the perimeter of the identified spawning area. Nets were checked at approximately 1 hour intervals and captured fish were cut from the inner mesh panel and placed in a mesh cage and processed within 2 hours. Suckers were identified by species and sex, measured to the nearest mm ( fork length), inspected for tags ( both PIT and Floy tags), and examined for physical afflictions ( e. g., presence oiLernaea spp. and lamprey scars). If a sucker did not have a PIT tag, one was inserted with a hypodermic needle along the ventral surface 1- 2 cm anterior of the pelvic girdle. The catch per unit effort ( CPUE) of adult Lost River suckers was calculated for individual sampling locations for each evening sampled. Because identified spawning areas varied in size we used different length trammel nets to encompass the spawning areas. We did not attempt to standardize CPUE based on length of trammel nets used at each location. Results We sampled shoreline spawning areas from 5 April - 17 June capturing a total of 808 Lost River suckers and 19 shortnose suckers from 5 sites ( Table 1). Lost River and shortnose suckers were captured at Sucker Springs, Silver Building Springs, Ouxy Springs, and Cinder Flats, while only Lost River suckers were captured at Boulder Springs. No suckers were captured at Barkley Springs and Modoc Point ( Table 1). The majority of Lost River suckers were captured at Cinder Flats ( 35%) and Sucker Springs ( 34%; Figure 2). Males dominated the catch at all sites and were generally smaller ( mean length = 538 mm) than females captured ( mean length = 596 mm). In particular, sex ratios ( males to females) were most skewed at Cinder Flats and Silver Building Springs ( Figure 3). Large females (> 650 mm) were captured at most sites, except Boulder Springs, and the size range offish captured over time remained similar with the exception that a fewer large individuals (> 600 mm) were captured in the late sampling period ( 1 May - 17 June) as compared to the early sampling period ( 6- 30 April; Figure 4; Appendix Figure A). The catch of shortnose suckers was limited at all sites sampled. Most ( 12 of 19) of the shortnose suckers were collected at Sucker Springs, with 1- 3 fish captured at Cinder Flats, Ouxy Springs, and Silver Building Springs ( Table 1). We identified 8 males and 8 females during the sampling period and were unable to determine sex for three individuals. The mean size of shortnose suckers was 360 mm ( range 289- 528 mm) similar to data reported by Perkins et al. ( In preparation) from Sucker, Silver Building, and Ouxy springs. We observed the highest CPUE of Lost River suckers at Cinder Flats ( mean CPUE= 12.7/ h) followed by Sucker Springs ( mean CPUE= 6.0/ h), Silver Building Springs ( mean CPUE = 2.8/ h), and Ouxy Springs ( mean CPUE= 2.4/ h) ( Figure 5). On three occasions at Cinder Flats, 20 or more suckers were captured within an hour or less resulting in the termination of sampling for the evening. CPUE was calculated for sampling dates at Boulder Springs ( mean CPUE= 1.4/ h), although comparisons with other sites is not applicable because this site was not initially included in systematic sampling efforts. We did not calculate CPUE for shortnose suckers. We captured a total of 32 Lost River and 2 shortnose suckers that were tagged during previous years sampling efforts. The majority ( 96%) of these fish was originally tagged at shoreline locations ( Table 2), which is consistent with historical recapture data ( Appendix Table A). Two Lost River suckers were originally tagged at Ball Point in UKL in July, after the spawning season. In addition, most Lost River suckers were recaptured before 1 May, including 15 fish that were collected at Sucker Springs during two sampling occasions in March ( Figure 6). We also recaptured a total of 21 Lost River suckers that were tagged in 1999 at shoreline spawning areas. Approximately half of these fish were recaptured at different areas than where they were tagged, indicating that some suckers are moving between spawning areas within the season ( Table 3). Discussion Our sampling indicated the spawning period for Lost River suckers lasted from mid- March through the beginning of June at shoreline spawning areas in 1999. The catch of Lost River suckers was dominated by males at all sites sampled, particularly at Cinder Flats and Silver Building Springs. Perkins et al., ( In preparation) reported skewed sex ratios at shoreline spawning locations following the fish kills that occurred in UKL from 1995- 1997. However, the ratios we observed were considerably higher than those reported by Perkins et al., ( In preparation). At this time we are unable to determine the reason for the sex ratios observed. It is possible that males remain longer at the spawning areas than females making them more vulnerable to capture. Perkins et al., ( In preparation) observed spawning acts and reported that males remained near the actual site where spawning occurs while females move onto the spawning site only when ready to spawn. We captured 23 Lost River suckers twice in 1999 and all but one of these fish were males. However, it is difficult to determine if this percentage is due to males remaining at these sites longer than females or a reflection of the existing sex ratios. Another possible explanation could be the large numbers of males in the catch are from the 1991- 1993 year classes and females from these year classes have yet to be recruited into the adult population. The majority of males captured ( 81%) were between 475 - 574 mm. Age and growth information from Lost River suckers collected during the 1996- 1997 fish kills indicate these fish would be between 5- 9 years old ( USGS, BRD, 10 unpublished data). Perkins et al., ( In preparation) reported that male Lost River suckers migrating up the Williamson River begin to be recruited into the adult population starting at age 4+, while females did not begin to mature until age 7+ . These data were based on examining length frequency distributions and noting when fish from the 1991 year class, which is presumed to be a strong year class, began showing up in trammel net catches. Fish from the 1991 year class would have been age 8+ in 1999. Buettner and Scoppetone ( 1990) examined opercles from Lost River suckers collected during the 1986 fish kill in UKL and reported that individuals matured between 6- 14 years of age with the peak being 9 years. It is possible that in the next few years more females from the 1991- 93 year classes will be recruited into the adult population spawning at shoreline areas. Our data provides additional evidence that distinct stocks of Lost River suckers may exist based on fidelity to spawning area. Of the 32 suckers we recaptured from previous years sampling efforts, all but two were originally tagged at shoreline spawning locations. The two fish that were not originally tagged at shoreline spawning locations were captured at Ball Point in July and were not presumed to be spawning in this location. Perkins et al. ( In preparation) reported that of 316 Lost River and 11 shortnose suckers recaptured at shoreline spawning areas all were originally tagged at shoreline spawning locations. Continuation of systematic sampling at both shoreline spawning areas and the Williamson and Sprague rivers will continue to provide information on potential separation of spawning populations. The majority of recaptured fish were tagged during the first half of our sampling efforts including 13 fish that were recaptured on 25 March while sampling with Larry Dunsmoor of the Klamath Tribes. Historically, the majority of sampling effort at 11 shoreline spawning locations occurred prior to 1 May, which may explain why most recaptures were collected during the early part of our sampling period. In fiiture years, we plan to continue systematic sampling through June to determine if temporal aspects of spawning remain consistent between years. The size offish captured at shoreline spawning areas decreased as the spawning season progressed, particularly near the end of our sampling period, although the decrease was not as dramatic as reported by Perkins et al., ( In preparation). It is possible that individual timing of Lost River sucker spawning is affected by size. Scoppettone et al., ( 1986) observed that smaller, younger cui- ui ( Chasmistes cujus) at Pyramid Lake spawned at the end of the spawning season. We believe further investigation is needed to determine if differences in spawning timing among individuals is due to size or related to stock differences. A limited number of shortnose suckers were captured in 1999. Sampling continued well into June and was sufficient to detect spawning concentrations of shortnose suckers at these sites. Based on previous sampling conducted at shoreline spawning areas, there appears to be a decreasing trend in the number of shortnose suckers captured at these sites ( Perkins, et al., In preparation). Our sampling efforts at shoreline spawning areas on the east side of UKL represents the first time these areas have been systematically sampled during the spawning season. Continuation of systematic sampling at these areas is important to provide information on species composition, timing and duration of spawning, fidelity to spawning areas, sex ratios, size distribution, and relative abundance. How these 12 population characteristics change over time will also provide important insights into the population stability of Lost River and shortnose suckers in UKL. 13 Literature Cited Buettner, M. And G. Scoppettone. 1990. Life history status of catostomids in Upper Klamath Lake, Oregon. U. S. F. W. S. Completion Report. 108 pp. Goldman, C. R. and A. J. Home. 1983. Limnology. McGraw Hill, New York. Moyle, P. B. 1976. Inland fishes of California. University of California Press, Berkeley, CA. Perkins, D. L., G. G. Scoppettone, and M. Buettner. In preparation. Reproductive biology and demographics of endangered Lost River and shortnose suckers in Upper Klamath Lake, Oregon. U. S. Fish and Wildlife Service. 1993. Lost River ( Deltistes luxatus) and shortnose ( Chasmistes brevirostris) sucker recovery plan. Portland, Oregon. 108 pp. 14 Table 1. Summary of the shoreline locations sampled in Upper Klamath Lake and the number of Lost River ( LRS) and shortnose ( SNS) suckers captured in 1999. Sampling Dates Sampled Number of days Number of LRS Number of SNS Location ( range) Sampled Captured Captured Barkley Springs 4/ 5- 4/ 27 4 0 0 11 21 0 19 284 2 4 0 0 20 129 3 19 100 2 Sucker Springs 4/ 5- 6/ 17 20 274 13 Total 808 20 Boulder Springs Cinder Flats Modoc Point Ouxy Springs Silver Bldg. Springs 4/ 27- 4/ 6- 4/ 13- 4/ 6- 4/ 5- 6/ 17 6/ 17 4/ 21 6/ 17 6/ 17 15 Table 2. Summary of the number of Lost River suckers recaptured from previous years sampling efforts at shoreline spawning locations in Upper Klamath Lake, 1999. Site Originally Captured Boulder Springs Cinder Flats Ouxy Springs Silver Bldg. Springs Sucker Springs Ball Point Total Boulder Springs 0 0 0 0 0 0 0 Site Cinder Flats 0 1 0 0 4 2 7 Recaptured Ouxy Springs 0 0 0 1 1 0 2 in 1999 Silver Bldg. Springs 0 0 0 1 0 0 1 Sucker Springs 0 0 1 2 19 0 22 16 Table 3. Summary of the number of Lost River suckers recaptured at shoreline locations in Upper Klamath Lake originally tagged in 1999. Site Originally Captured in 1999 Boulder Springs Cinder Flats Ouxy Springs Silver Bldg. Springs Sucker Springs Total Boulder Springs 0 0 0 0 0 0 Site Cinder Flats 0 3 1 3 1 8 Recaptured Ouxy Springs 0 1 0 0 3 4 in 1999 Silver Bldg. Springs 0 0 1 1 0 2 Sucker Springs 0 2 0 1 6 9 17 1. Sucker Springs 2. Silver Building Springs 3. Ouxy Springs 4. Cinder Flats 5. Boulder Springs Figure 1. Map of Upper Klamath and Agency Lakes showing major tributaries and shoreline spawning areas sampled in 1999. 18 o I 50 45 40 35 30 25 20 15 10 5 0 BOULDER SPRINGS 50 45 40 35 30 25 20 15 10 5 0 D LRS Male • LRS Female * No Fish Jtt * * * * * * OUXY SPRINGS D LRS Male • LRS Female * No Fish 50 45 40 35 30 25 20 15 10 5 0 CINDER FLATS D LRS Unknow n _ r i • LRS Male • i_ r\ o remaie ic No Fish EII1IJ n „ * * * * 50 45 40 35 30 25 20 15 10 5 0 > SILVER BUILDING SPRINGS • LRS Unknow n • LRS Male • LRS Female * No Fish D n n p » * * * * * SUCKER SPRINGS ALL AREAS COMBINED • LRS Unknown D LRS Male • LRS Female • LRS Unknow n • LRS Male • LRS Female / / / / / / Figure 2. Summary of the number and sex of Lost River Suckers ( LRS) captured at shoreline spawning areas in Upper Klamath Lake, 1999 sampling. LRS unknown refers to captured individuals in which sex could not be determined. 19 70% -, 60% 50% 40% - 30% - 20% - 10% 0% CINDER FLATS _ o_ n= 283 9.1 : 1 8C O in io in om CD o i n 70% -, 60% - 50% - 40% - 30% - 20% - 10% - 0% - BOULDER SPRINGS y n 11 7 6 2 n= 21 9.5: 1 • g si n 8 CD omr o in oo § 70% 60% 50% 40% 30% 20% 10% 0% OUXY SPRINGS om CN oi n co o ini o in in SUCKER SPRINGS 70% -, 60% - 50% - 40% - 30% - 20% - 10% - 0% - n= 129 4.1 : 0 • _ o in CD omh omoo n= 273 3.5: 1 U • - - sC O oi n oi nm om o i n 00 70% 60% 50% 40% 30% 20% - 10% 0% SILVER BUILDING SPRINGS 70% 60% - 50% - 40% 30% 20% 10% - 0% 8 CM ALL SITES 8 CO JL 8 8 i n n= 99 8.1 : 1 • H „ - in in in CD h- 00 n= 805 5.3: 1 _ D • Male • Female 8 C N O O O O O O O O O O O i n o m oin i nin oCDi nCDo i n o i nco Fork length Figure 3. Length frequency histogram of male and female Lost River suckers ( LRS) captured at shore-line spawning areas in Upper Klamath Lake, 1999. The total number of LRS captured in 1999 and ratio of males to females are presented in the upper right hand corner of each graph. 20 E QJ D 160 i 140 120 100 80 60 40 20 0 A) 1999 LR Length Frequency ( 3/ 18/ 99- 4/ 30/ 99) DMale • Female • male = 457 xM = 541.4 i siaev - jo. y female = 60 xF = 611.9 stdev = 77.2 (—\| Qy O ^ D 160 140 120 100 80 60 40 20 # 4? B) o - I— # $ # C) # # $ # 1999 LR Length Frequency ( 5/ 1/ 99 - 6/ 8/ 99) DMale • Female male = 219 xM = 531.4 5> lUeV — H 1 , , — i remaie = bB xF = 582 8 stdev = 68.1 • y . _ _ # ^ # # # # # # # ^ 1999 SN Length Frequency ( 4/ 30/ 99 - 5/ 30/ 99) 1 U 14 - 12 - 10 s p. A 2 0 - , Dmale • female y y • l i y n male = 8 xM = 363 stdev - 29.7 fpryiolp — ft xF = 357.1 stdev = 35.5 Forklength ( mm) Figure 4. Length frequency for Lost River ( LRS) and shortnose ( SNS) suckers captured at shoreline spawning areas in Upper Klamath Lake, 1999. Graphs represent A) LRS caught from March 19- April 30, 1999, B) LRS caught from May 1- June 8, 1999, and C) SNS caught from April 30- May 30, 1999 ( all SNS sampling days were combined due to limited SNS numbers). Four LRS with unknown gender were not included in the graph, two were caught before May 1st, and two after May 1st. Three SNS with unknown gender were not included in the graph. 21 BOULDER SPRINGS 20 i 18 16 - I 14 12 10 8 6 4 2 0 O) O) O) 0 ) 0 ) 0 ) 0 ) 0 ) in CM O) $ § I co o L? 5 LO O) O) O) g> g> g> o r^ •<• n ^ CN CD CD CD 45 40 - 35 30 25 20 15 10 - 5 0 CINDER FLATS 0 ) 0 ) OO - f - r in in 0 ) 0 ) 0 ) C D C D C D 1 sw 20 18 16- 14- 12 - 10 8 6 4 OUXYSPRNGS Jl 0 ) 0 ) 0 ) 0 ) OO 0 ) 0 ) 0 ) C N I O C D O) O) O) O) Q < o z: ? z in CD CD 20- 18 - 16 14 - 12 - 10 - 8 6 4 - 2 - 0 - SILVER BUILDING SPRINGS ii , II p l, « u u •———,—— O) O) O) 0 ) 0 ) 0 ) in CN O) T- CM CM O) O) O) O) O) O) CO O h » - in O) O) O) ill CD CD CD SUCKER SPRINGS ALL SITES Figure 5. Summary of catch per unit effort ( CPUE) of Lost River suckers at shoreline spawning areas in Upper Klamath Lake, 1999. Note change in scale for the Cinder Flats and the All Sites graphs. 22 BOULDER SPRINGS 14 12 10 8 -\| 6 4 2 0 n= 0 0 ) 0 ) 0 ) 0 ) 0 ) 0 ) 0 ) O) CD CN O) CD CO O T - C\\| ^ ^ T- CNJ CO CO CO ^" ^" ^" OUXY SPRINGS 1 C D n= 2 14 1 8 4 2^ 0 oo S ^ ^ SUCKER SPRINGS ^ £ j CNJ in in to n= 22 - U-CD CO O j - CM CO 1 C D 14 12 -\ 10 8 -] 6 4 2 - 0 CINDER FLATS n= 7 LJl 0 ) 0 ) 0 ) 0 ) 0 ) T^ Cr^ N ^? ^ T- 14 12 10 - 8 6 4 - 2 0 SILVER BUILDING SPRINGS Tt x- 00 - CN CN in in in n= 1 0 ) 0 ) 0 ) 0 ) 0 ) 0 ) 0 ) 0 ) 0 ) 0 ) 0 ) 0 ) O) CD CN O> CD CO ^ CJ ^ ^ ^ CN co co ^ j- "< t ALL SITES O) O) O) O) O) O) in in in n= 32 I 0 0) in in in Figure 6. Summary of the number of Lost River suckers recaptured at shoreline spawning areas, Upper Klamath Lake, 1999. Recaptured fish were originally tagged betweeen 1988- 1998. 23 Appendix Table A. Summary of recapture data for Lost River Suckers in the Upper Klamath Lake Basin from 1985- 1999. Sampling was generally conducted from March- July of each year, although the emphasis in sampling was during the spawning period. Recapture data includes fish that were tagged with Floy and PIT tags. Site Last Recaptured Site Originally Captured Cinder Flats Ouxy Springs Silver Bldg. Springs Sucker Springs Williamson River Sprague River Upper Lake Middle Lake Total Cinder Flats 1 0 0 4 0 0 2 0 7 Ouxy Springs 0 1 1 1 0 0 0 0 3 Silver Bldg. Springs 0 0 1 6 0 0 0 0 7 Sucker Springs 0 0 6 288 4 0 0 0 298 Williamson River 0 0 0 1 6 3 0 0 10 Sprague River 0 0 0 0 1 13 1 0 15 Upper Lake 0 0 0 0 0 0 0 0 0 Middle Lake 0 0 1 0 1 0 0 0 2 Total 1 1 9 300 12 16 3 0 342 Appendix Table B. Summary of recapture data for shortnose suckers in the Upper Klamath Lake Basin from 1985- 1999. Sampling was generally conducted from March- July of each year, although the emphasis in sampling was during the spawning period. Recapture data includes fish that were tagged with Floy and PIT tags. Site Last Recaptured Site Originally Captured Ouxy Springs Silver Bldg. Springs Sucker Springs Williamson River Sprague River Lower Lake Middle Lake Total Ouxy Springs 1 0 0 0 0 0 0 1 Silver Bldg. Springs 0 0 0 0 0 0 0 0 Sucker Springs 1 0 0 0 0 0 0 1 Williamson River 0 0 0 4 0 0 0 4 Sprague River 0 0 0 2 3 0 0 5 Lower Lake 0 0 0 0 0 0 0 0 Middle Lake 0 0 0 1 2 0 5 8 Upper Lake 0 0 0 0 0 0 0 0 Reeder Road Bridge 0 0 0 0 0 0 1 1 Total 2 0 0 7 5 0 6 20 25 5 2iu5 Appendix Figure A. Summary of the size range of Lost River suckers captured at shoreline sampling areas in Upper Klamath Lake, 1999, by date sampled. Title: Monitoring of Lost River and Shortnose suckers and shoreline spawning areas in Upper Klamath Lake, 1999 Author: Shively, Rip S.; Bautista, Mark F.; Kohler, Andre E. Year: 1999, 2005 Monitoring of Lost River and Shortnose Suckers at Shoreline Spawning Areas in Upper Klamath Lake, 1999 Prepared by: Rip S. Shively1 Mark F. Bautista2 Andre E. Kohler2 1 U. S. Geological Survey, Biological Resources Division Klamath Falls Duty Station 6937 Washburn Way Klamath Falls, OR 97603 2 Johnson Controls World Services Inc. NERC Operation Post Office Box 270308 Fort Collins, CO 80527 Executive Summary In 1999, we sampled Lost River { Deltistes luxatus) and shortnose ( Chasmistes brevirostris) suckers from 5 April to 17 June at five shoreline spawning locations in Upper Klamath Lake ( UKL). Trammel nets were set to encompass identified spawning areas and were fished approximately 1- 1.5 hours before sunset until 3 hours after sunset or until 20 or more fish were captured. A total of 808 Lost River and 19 shortnose suckers were captured from Sucker, Silver Building, Ouxy, and Boulder springs, and Cinder Flats. The majority of Lost River suckers were captured at Cinder Flats ( 35%) and Sucker Springs ( 34%), followed by Ouxy Springs ( 16%), Silver Building Springs ( 12%), and Boulder Springs ( 3%). Males dominated the catch at all sites, but the sex ratios at Cinder Flats and Silver Building Springs were particularly skewed towards males. We recaptured 32 Lost River suckers that had been tagged during previous years sampling efforts. All of these fish, with the exception of two fish tagged at Ball Point in July, were originally tagged during the spawning season at shoreline spawning areas in UKL. This information provides further evidence that distinct stocks of Lost River suckers exist based on spawning location ( i. e., UKL and Williamson River). We also recaptured 23 Lost River suckers that were tagged in 1999 at shoreline spawning areas. Approximately half of these fish were recaptured at different locations than tagged indicating these fish were moving between spawning areas. The size offish captured at shoreline spawning areas decreased as the spawning season progressed, although the decrease in size was not as dramatic as reported in previous years. A limited number of shortnose suckers were captured at shoreline spawning areas in 1999, with a majority sampled after 1 May. Previous data for shortnose suckers at these sites is limited with respect to size, timing of spawning, sex composition, and relative numbers. Continuation of systematic sampling efforts at shoreline spawning areas will provide valuable information on the demographics and life history of Lost River and shortnose suckers utilizing these areas. Acknowledgements We thank Anita Baker, Brooke Bechen, Lani Hickey, and Tonya Wiley for assisting with sampling offish at shoreline spawning areas. Mark Buettner and Brian Peck ( U. S. Bureau of Reclamation) provided support during the early phases of our sampling as well as helpful comments on this report. We also appreciate the cooperation and support of Larry Dunsmoor ( Klamath Tribes) for identifying spawning areas, providing logistical support, and for the thoughtful review of this report. Cassandra Watson and Elizabeth Neuman produced finalized versions of tables and figures within this report and their efforts are greatly appreciated. This research was funded by the U. S. Geological Survey, Biological Resources Division through the Western Reservoirs Initiative. Introduction Severe water quality problems in Upper Klamath Lake ( UKL) have led to critical fisheries concerns for the region. Historically, UKL was eutrophic but has become hypereutrophic ( Goldman and Home 1983) presumably due to land- use practices within the basin ( USFWS 1993). As a result, the algal community has shifted to a monoculture of the blue- green algae Aphanizomemon flos- aquae and massive blooms of this species have been directly related to poor water quality episodes in UKL. The growth and decomposition of dense algal blooms in the lake frequently cause extreme water quality conditions characterized by high pH ( 9- 10.5), widely variable dissolved oxygen ( anoxic to supersaturated), and high ammonia concentrations (> 0.5 mg/ 1 unionized). In addition to water quality problems associated with A. flos- aquae, it is believed the loss of marsh habitat near the lake, timber harvest, removal of riparian vegetation, livestock grazing, and agricultural practices within the basin has contributed to hypereutrophic conditions. It is likely that these disturbances have altered the UKL ecosystem substantially enough to contribute to the near monoculture of A. flos- aquae. Investigations in 1913 documented the algal community as a diverse mix of blue- green and diatom communities, however, by the 1950' s A. flos- aquae was dominant ( USFWS 1993). The Lost River sucker ( Deltistes luxatus) and shortnose sucker ( Chasmistes brevirostris) are endemic to the Upper Klamath Basin of California and Oregon ( Moyle 1976). Declining population trends for both species were noted as early as the mid- 1960' s, however, the severities of the population declines were not evident until the mid- 1980' s. In 1988 the U. S. Fish and Wildlife Service listed both Lost River and shortnose suckers as endangered. Suspected reasons for their decline included damming of rivers, dredging and draining of marshes, water diversions, hybridization, competition and predation by exotic species, insularization of habitat, and water quality problems associated with timber harvest, removal of riparian vegetation, livestock grazing, and agricultural practices ( USFWS 1993). The U. S. Geological Survey, Biological Resources Division ( BRD) has been conducting field investigations on Lost River and shortnose suckers in UKL since 1994. The majority of these sampling efforts have focused on catching fish in UKL and the Lower Williamson River. Sampling in the Lower Williamson River focused on developing indices of relative abundance of Lost River and shortnose suckers. In 1999, Oregon State University continued sampling in the Lower Williamson River fishing trammel nets from April to August at four standardized locations. In addition to sampling efforts in the Lower Williamson River, BRD crews conducted periodic sampling at several shoreline spawning areas on the east side of UKL. This sampling was beneficial because it provided information on species composition, size, and sex ratios of suckers utilizing these areas. However, temporal changes in abundance may have been missed because consistent sampling never occurred throughout the entire spawning season ( Perkins et al, In preparation). Recently, there has been increased concern on the effects of water level management in UKL on spawning suckers. Information is needed on the timing, relative abundance, and distribution of sucker spawning in UKL to make informed decisions with respect to management of lake elevation. In 1999, we conducted systematic trammel netting surveys at Sucker, Silver Building, Ouxy, and Boulder springs and Cinder Flats along the east shore of UKL. In addition, we sampled periodically at Barkley Springs and Modoc Point to determine if suckers were utilizing these areas for spawning. This report summarizes data collected in 1999 on shoreline spawning populations of Lost River and shortnose suckers with emphasis on timing, species composition, sex ratios, and relative abundance. Methods We conducted systematic trammel netting surveys at five locations along the east shore of UKL ( Figure 1). We began sampling at Cinder Flats, Sucker, Silver Building, and Ouxy springs in early April with Boulder Springs added to the list of sampling sites on 27 April. In addition to these sites, we periodically sampled at Barkley Springs and Modoc Point ( Table 1). We attempted to sample each site twice per week although certain sites were only sampled once per week when catch rates of suckers were low ( i. e., less than 5 fish per evening). Trammel nets were fished for about 4 hours ( approximately 1- 1.5 hours before sunset until 3 hours after dark) or until we captured 20 or more fish. Nets used at individual sites varied in length from 15- 30 m, were 1.8 m tall with two outer panels ( 30cm bar mesh), an inner panel ( 3.8 cm bar mesh), a foam core float line, and a lead core bottom line. Generally, we set 1- 2 nets starting at the shoreline and extending out to encompass the perimeter of the identified spawning area. Nets were checked at approximately 1 hour intervals and captured fish were cut from the inner mesh panel and placed in a mesh cage and processed within 2 hours. Suckers were identified by species and sex, measured to the nearest mm ( fork length), inspected for tags ( both PIT and Floy tags), and examined for physical afflictions ( e. g., presence oiLernaea spp. and lamprey scars). If a sucker did not have a PIT tag, one was inserted with a hypodermic needle along the ventral surface 1- 2 cm anterior of the pelvic girdle. The catch per unit effort ( CPUE) of adult Lost River suckers was calculated for individual sampling locations for each evening sampled. Because identified spawning areas varied in size we used different length trammel nets to encompass the spawning areas. We did not attempt to standardize CPUE based on length of trammel nets used at each location. Results We sampled shoreline spawning areas from 5 April - 17 June capturing a total of 808 Lost River suckers and 19 shortnose suckers from 5 sites ( Table 1). Lost River and shortnose suckers were captured at Sucker Springs, Silver Building Springs, Ouxy Springs, and Cinder Flats, while only Lost River suckers were captured at Boulder Springs. No suckers were captured at Barkley Springs and Modoc Point ( Table 1). The majority of Lost River suckers were captured at Cinder Flats ( 35%) and Sucker Springs ( 34%; Figure 2). Males dominated the catch at all sites and were generally smaller ( mean length = 538 mm) than females captured ( mean length = 596 mm). In particular, sex ratios ( males to females) were most skewed at Cinder Flats and Silver Building Springs ( Figure 3). Large females (> 650 mm) were captured at most sites, except Boulder Springs, and the size range offish captured over time remained similar with the exception that a fewer large individuals (> 600 mm) were captured in the late sampling period ( 1 May - 17 June) as compared to the early sampling period ( 6- 30 April; Figure 4; Appendix Figure A). The catch of shortnose suckers was limited at all sites sampled. Most ( 12 of 19) of the shortnose suckers were collected at Sucker Springs, with 1- 3 fish captured at Cinder Flats, Ouxy Springs, and Silver Building Springs ( Table 1). We identified 8 males and 8 females during the sampling period and were unable to determine sex for three individuals. The mean size of shortnose suckers was 360 mm ( range 289- 528 mm) similar to data reported by Perkins et al. ( In preparation) from Sucker, Silver Building, and Ouxy springs. We observed the highest CPUE of Lost River suckers at Cinder Flats ( mean CPUE= 12.7/ h) followed by Sucker Springs ( mean CPUE= 6.0/ h), Silver Building Springs ( mean CPUE = 2.8/ h), and Ouxy Springs ( mean CPUE= 2.4/ h) ( Figure 5). On three occasions at Cinder Flats, 20 or more suckers were captured within an hour or less resulting in the termination of sampling for the evening. CPUE was calculated for sampling dates at Boulder Springs ( mean CPUE= 1.4/ h), although comparisons with other sites is not applicable because this site was not initially included in systematic sampling efforts. We did not calculate CPUE for shortnose suckers. We captured a total of 32 Lost River and 2 shortnose suckers that were tagged during previous years sampling efforts. The majority ( 96%) of these fish was originally tagged at shoreline locations ( Table 2), which is consistent with historical recapture data ( Appendix Table A). Two Lost River suckers were originally tagged at Ball Point in UKL in July, after the spawning season. In addition, most Lost River suckers were recaptured before 1 May, including 15 fish that were collected at Sucker Springs during two sampling occasions in March ( Figure 6). We also recaptured a total of 21 Lost River suckers that were tagged in 1999 at shoreline spawning areas. Approximately half of these fish were recaptured at different areas than where they were tagged, indicating that some suckers are moving between spawning areas within the season ( Table 3). Discussion Our sampling indicated the spawning period for Lost River suckers lasted from mid- March through the beginning of June at shoreline spawning areas in 1999. The catch of Lost River suckers was dominated by males at all sites sampled, particularly at Cinder Flats and Silver Building Springs. Perkins et al., ( In preparation) reported skewed sex ratios at shoreline spawning locations following the fish kills that occurred in UKL from 1995- 1997. However, the ratios we observed were considerably higher than those reported by Perkins et al., ( In preparation). At this time we are unable to determine the reason for the sex ratios observed. It is possible that males remain longer at the spawning areas than females making them more vulnerable to capture. Perkins et al., ( In preparation) observed spawning acts and reported that males remained near the actual site where spawning occurs while females move onto the spawning site only when ready to spawn. We captured 23 Lost River suckers twice in 1999 and all but one of these fish were males. However, it is difficult to determine if this percentage is due to males remaining at these sites longer than females or a reflection of the existing sex ratios. Another possible explanation could be the large numbers of males in the catch are from the 1991- 1993 year classes and females from these year classes have yet to be recruited into the adult population. The majority of males captured ( 81%) were between 475 - 574 mm. Age and growth information from Lost River suckers collected during the 1996- 1997 fish kills indicate these fish would be between 5- 9 years old ( USGS, BRD, 10 unpublished data). Perkins et al., ( In preparation) reported that male Lost River suckers migrating up the Williamson River begin to be recruited into the adult population starting at age 4+, while females did not begin to mature until age 7+ . These data were based on examining length frequency distributions and noting when fish from the 1991 year class, which is presumed to be a strong year class, began showing up in trammel net catches. Fish from the 1991 year class would have been age 8+ in 1999. Buettner and Scoppetone ( 1990) examined opercles from Lost River suckers collected during the 1986 fish kill in UKL and reported that individuals matured between 6- 14 years of age with the peak being 9 years. It is possible that in the next few years more females from the 1991- 93 year classes will be recruited into the adult population spawning at shoreline areas. Our data provides additional evidence that distinct stocks of Lost River suckers may exist based on fidelity to spawning area. Of the 32 suckers we recaptured from previous years sampling efforts, all but two were originally tagged at shoreline spawning locations. The two fish that were not originally tagged at shoreline spawning locations were captured at Ball Point in July and were not presumed to be spawning in this location. Perkins et al. ( In preparation) reported that of 316 Lost River and 11 shortnose suckers recaptured at shoreline spawning areas all were originally tagged at shoreline spawning locations. Continuation of systematic sampling at both shoreline spawning areas and the Williamson and Sprague rivers will continue to provide information on potential separation of spawning populations. The majority of recaptured fish were tagged during the first half of our sampling efforts including 13 fish that were recaptured on 25 March while sampling with Larry Dunsmoor of the Klamath Tribes. Historically, the majority of sampling effort at 11 shoreline spawning locations occurred prior to 1 May, which may explain why most recaptures were collected during the early part of our sampling period. In fiiture years, we plan to continue systematic sampling through June to determine if temporal aspects of spawning remain consistent between years. The size offish captured at shoreline spawning areas decreased as the spawning season progressed, particularly near the end of our sampling period, although the decrease was not as dramatic as reported by Perkins et al., ( In preparation). It is possible that individual timing of Lost River sucker spawning is affected by size. Scoppettone et al., ( 1986) observed that smaller, younger cui- ui ( Chasmistes cujus) at Pyramid Lake spawned at the end of the spawning season. We believe further investigation is needed to determine if differences in spawning timing among individuals is due to size or related to stock differences. A limited number of shortnose suckers were captured in 1999. Sampling continued well into June and was sufficient to detect spawning concentrations of shortnose suckers at these sites. Based on previous sampling conducted at shoreline spawning areas, there appears to be a decreasing trend in the number of shortnose suckers captured at these sites ( Perkins, et al., In preparation). Our sampling efforts at shoreline spawning areas on the east side of UKL represents the first time these areas have been systematically sampled during the spawning season. Continuation of systematic sampling at these areas is important to provide information on species composition, timing and duration of spawning, fidelity to spawning areas, sex ratios, size distribution, and relative abundance. How these 12 population characteristics change over time will also provide important insights into the population stability of Lost River and shortnose suckers in UKL. 13 Literature Cited Buettner, M. And G. Scoppettone. 1990. Life history status of catostomids in Upper Klamath Lake, Oregon. U. S. F. W. S. Completion Report. 108 pp. Goldman, C. R. and A. J. Home. 1983. Limnology. McGraw Hill, New York. Moyle, P. B. 1976. Inland fishes of California. University of California Press, Berkeley, CA. Perkins, D. L., G. G. Scoppettone, and M. Buettner. In preparation. Reproductive biology and demographics of endangered Lost River and shortnose suckers in Upper Klamath Lake, Oregon. U. S. Fish and Wildlife Service. 1993. Lost River ( Deltistes luxatus) and shortnose ( Chasmistes brevirostris) sucker recovery plan. Portland, Oregon. 108 pp. 14 Table 1. Summary of the shoreline locations sampled in Upper Klamath Lake and the number of Lost River ( LRS) and shortnose ( SNS) suckers captured in 1999. Sampling Dates Sampled Number of days Number of LRS Number of SNS Location ( range) Sampled Captured Captured Barkley Springs 4/ 5- 4/ 27 4 0 0 11 21 0 19 284 2 4 0 0 20 129 3 19 100 2 Sucker Springs 4/ 5- 6/ 17 20 274 13 Total 808 20 Boulder Springs Cinder Flats Modoc Point Ouxy Springs Silver Bldg. Springs 4/ 27- 4/ 6- 4/ 13- 4/ 6- 4/ 5- 6/ 17 6/ 17 4/ 21 6/ 17 6/ 17 15 Table 2. Summary of the number of Lost River suckers recaptured from previous years sampling efforts at shoreline spawning locations in Upper Klamath Lake, 1999. Site Originally Captured Boulder Springs Cinder Flats Ouxy Springs Silver Bldg. Springs Sucker Springs Ball Point Total Boulder Springs 0 0 0 0 0 0 0 Site Cinder Flats 0 1 0 0 4 2 7 Recaptured Ouxy Springs 0 0 0 1 1 0 2 in 1999 Silver Bldg. Springs 0 0 0 1 0 0 1 Sucker Springs 0 0 1 2 19 0 22 16 Table 3. Summary of the number of Lost River suckers recaptured at shoreline locations in Upper Klamath Lake originally tagged in 1999. Site Originally Captured in 1999 Boulder Springs Cinder Flats Ouxy Springs Silver Bldg. Springs Sucker Springs Total Boulder Springs 0 0 0 0 0 0 Site Cinder Flats 0 3 1 3 1 8 Recaptured Ouxy Springs 0 1 0 0 3 4 in 1999 Silver Bldg. Springs 0 0 1 1 0 2 Sucker Springs 0 2 0 1 6 9 17 1. Sucker Springs 2. Silver Building Springs 3. Ouxy Springs 4. Cinder Flats 5. Boulder Springs Figure 1. Map of Upper Klamath and Agency Lakes showing major tributaries and shoreline spawning areas sampled in 1999. 18 o I 50 45 40 35 30 25 20 15 10 5 0 BOULDER SPRINGS 50 45 40 35 30 25 20 15 10 5 0 D LRS Male • LRS Female No Fish Jtt * * * * * * OUXY SPRINGS D LRS Male • LRS Female * No Fish 50 45 40 35 30 25 20 15 10 5 0 CINDER FLATS D LRS Unknow n _ r i • LRS Male • i_ r\ o remaie ic No Fish EII1IJ n „ * * * * 50 45 40 35 30 25 20 15 10 5 0 > SILVER BUILDING SPRINGS • LRS Unknow n • LRS Male • LRS Female * No Fish D n n p » * * * * * SUCKER SPRINGS ALL AREAS COMBINED • LRS Unknown D LRS Male • LRS Female • LRS Unknow n • LRS Male • LRS Female / / / / / / Figure 2. Summary of the number and sex of Lost River Suckers ( LRS) captured at shoreline spawning areas in Upper Klamath Lake, 1999 sampling. LRS unknown refers to captured individuals in which sex could not be determined. 19 70% -, 60% 50% 40% - 30% - 20% - 10% 0% CINDER FLATS _ o_ n= 283 9.1 : 1 8C O in io in om CD o i n 70% -, 60% - 50% - 40% - 30% - 20% - 10% - 0% - BOULDER SPRINGS y n 11 7 6 2 n= 21 9.5: 1 • g si n 8 CD omr o in oo § 70% 60% 50% 40% 30% 20% 10% 0% OUXY SPRINGS om CN oi n co o ini o in in SUCKER SPRINGS 70% -, 60% - 50% - 40% - 30% - 20% - 10% - 0% - n= 129 4.1 : 0 • _ o in CD omh omoo n= 273 3.5: 1 U • - - sC O oi n oi nm om o i n 00 70% 60% 50% 40% 30% 20% - 10% 0% SILVER BUILDING SPRINGS 70% 60% - 50% - 40% 30% 20% 10% - 0% 8 CM ALL SITES 8 CO JL 8 8 i n n= 99 8.1 : 1 • H „ - in in in CD h- 00 n= 805 5.3: 1 _ D • Male • Female 8 C N O O O O O O O O O O O i n o m oin i nin oCDi nCDo i n o i nco Fork length Figure 3. Length frequency histogram of male and female Lost River suckers ( LRS) captured at shore-line spawning areas in Upper Klamath Lake, 1999. The total number of LRS captured in 1999 and ratio of males to females are presented in the upper right hand corner of each graph. 20 E QJ D 160 i 140 120 100 80 60 40 20 0 A) 1999 LR Length Frequency ( 3/ 18/ 99- 4/ 30/ 99) DMale • Female • male = 457 xM = 541.4 i siaev - jo. y female = 60 xF = 611.9 stdev = 77.2 (—\| Qy O ^ D 160 140 120 100 80 60 40 20 # 4? B) o - I— # $ # C) # # $ # 1999 LR Length Frequency ( 5/ 1/ 99 - 6/ 8/ 99) DMale • Female male = 219 xM = 531.4 5> lUeV — H 1 , , — i remaie = bB xF = 582 8 stdev = 68.1 • y . _ _ # ^ # # # # # # # ^ 1999 SN Length Frequency ( 4/ 30/ 99 - 5/ 30/ 99) 1 U 14 - 12 - 10 s p. A 2 0 - , Dmale • female y y • l i y n male = 8 xM = 363 stdev - 29.7 fpryiolp — ft xF = 357.1 stdev = 35.5 Forklength ( mm) Figure 4. Length frequency for Lost River ( LRS) and shortnose ( SNS) suckers captured at shoreline spawning areas in Upper Klamath Lake, 1999. Graphs represent A) LRS caught from March 19- April 30, 1999, B) LRS caught from May 1- June 8, 1999, and C) SNS caught from April 30- May 30, 1999 ( all SNS sampling days were combined due to limited SNS numbers). Four LRS with unknown gender were not included in the graph, two were caught before May 1st, and two after May 1st. Three SNS with unknown gender were not included in the graph. 21 BOULDER SPRINGS 20 i 18 16 - I 14 12 10 8 6 4 2 0 O) O) O) 0 ) 0 ) 0 ) 0 ) 0 ) in CM O) $ § I co o L? 5 LO O) O) O) g> g> g> o r^ •<*• n ^ CN CD CD CD 45 40 - 35 30 25 20 15 10 - 5 0 CINDER FLATS 0 ) 0 ) OO - f - r in in 0 ) 0 ) 0 ) C D C D C D 1 sw 20 18 16- 14- 12 - 10 8 6 4 OUXYSPRNGS Jl 0 ) 0 ) 0 ) 0 ) OO 0 ) 0 ) 0 ) C N I O C D O) O) O) O) Q < o z: ? z in CD CD 20- 18 - 16 14 - 12 - 10 - 8 6 4 - 2 - 0 - SILVER BUILDING SPRINGS ii , II p l, « u u •———,—— O) O) O) 0 ) 0 ) 0 ) in CN O) T- CM CM O) O) O) O) O) O) CO O h » - in O) O) O) ill CD CD CD SUCKER SPRINGS ALL SITES Figure 5. Summary of catch per unit effort ( CPUE) of Lost River suckers at shoreline spawning areas in Upper Klamath Lake, 1999. Note change in scale for the Cinder Flats and the All Sites graphs. 22 BOULDER SPRINGS 14 12 10 8 -\| 6 4 2 0 n= 0 0 ) 0 ) 0 ) 0 ) 0 ) 0 ) 0 ) O) CD CN O) CD CO O T - C\\| ^ ^ T- CNJ CO CO CO ^" ^" ^" OUXY SPRINGS 1 C D n= 2 14 1 8 4 2^ 0 oo S ^ ^ SUCKER SPRINGS ^ £ j CNJ in in to n= 22 - U-CD CO O j - CM CO 1 C D 14 12 -\ 10 8 -] 6 4 2 - 0 CINDER FLATS n= 7 LJl 0 ) 0 ) 0 ) 0 ) 0 ) T^ Cr^ N ^? ^ T- 14 12 10 - 8 6 4 - 2 0 SILVER BUILDING SPRINGS Tt x- 00 - CN CN in in in n= 1 0 ) 0 ) 0 ) 0 ) 0 ) 0 ) 0 ) 0 ) 0 ) 0 ) 0 ) 0 ) O) CD CN O> CD CO ^ CJ ^ ^ ^ CN co co ^ j- "< t ALL SITES O) O) O) O) O) O) in in in n= 32 I 0 0) in in in Figure 6. Summary of the number of Lost River suckers recaptured at shoreline spawning areas, Upper Klamath Lake, 1999. Recaptured fish were originally tagged betweeen 1988- 1998. 23 Appendix Table A. Summary of recapture data for Lost River Suckers in the Upper Klamath Lake Basin from 1985- 1999. Sampling was generally conducted from March- July of each year, although the emphasis in sampling was during the spawning period. Recapture data includes fish that were tagged with Floy and PIT tags. Site Last Recaptured Site Originally Captured Cinder Flats Ouxy Springs Silver Bldg. Springs Sucker Springs Williamson River Sprague River Upper Lake Middle Lake Total Cinder Flats 1 0 0 4 0 0 2 0 7 Ouxy Springs 0 1 1 1 0 0 0 0 3 Silver Bldg. Springs 0 0 1 6 0 0 0 0 7 Sucker Springs 0 0 6 288 4 0 0 0 298 Williamson River 0 0 0 1 6 3 0 0 10 Sprague River 0 0 0 0 1 13 1 0 15 Upper Lake 0 0 0 0 0 0 0 0 0 Middle Lake 0 0 1 0 1 0 0 0 2 Total 1 1 9 300 12 16 3 0 342 Appendix Table B. Summary of recapture data for shortnose suckers in the Upper Klamath Lake Basin from 1985- 1999. Sampling was generally conducted from March- July of each year, although the emphasis in sampling was during the spawning period. Recapture data includes fish that were tagged with Floy and PIT tags. Site Last Recaptured Site Originally Captured Ouxy Springs Silver Bldg. Springs Sucker Springs Williamson River Sprague River Lower Lake Middle Lake Total Ouxy Springs 1 0 0 0 0 0 0 1 Silver Bldg. Springs 0 0 0 0 0 0 0 0 Sucker Springs 1 0 0 0 0 0 0 1 Williamson River 0 0 0 4 0 0 0 4 Sprague River 0 0 0 2 3 0 0 5 Lower Lake 0 0 0 0 0 0 0 0 Middle Lake 0 0 0 1 2 0 5 8 Upper Lake 0 0 0 0 0 0 0 0 Reeder Road Bridge 0 0 0 0 0 0 1 1 Total 2 0 0 7 5 0 6 20 25 5 2iu5 Appendix Figure A. Summary of the size range of Lost River suckers captured at shoreline sampling areas in Upper Klamath Lake, 1999, by date sampled.

1596. [Image] Water quality conditions in Upper Klamath and Agency Lakes, Oregon, 2005


	Agency Lakes. Oregon. 2005 M.Wood By Gene R. Hoilman, Mary K. Lindenberg, and Tamara Abstract During June-October 2005, water quality data were collected from Upper Klamath and Agency Lakes In Oregon, ...
	Citation Citation Citation Abstract Copy Title: Water quality conditions in Upper Klamath and Agency Lakes, Oregon, 2005 Author: Hoilman, Gene R Year: 2008 Agency Lakes. Oregon. 2005 M.Wood By Gene R. Hoilman, Mary K. Lindenberg, and Tamara Abstract During June-October 2005, water quality data were collected from Upper Klamath and Agency Lakes In Oregon, and meteorological data were collected around and within Upper Klamath Lake. Data recorded at two continuous water quality monitors In Agency Lake showed similar temperature patterns throughout the field season, but data recorded at the northern site showed more day-to-day variability for dissolved oxygen concentration and saturation after late June and more day-to-day variability for pH and specific conductance values after mid-July. Data recorded from the northern and southern parts of Agency Lake showed more comparable day-to-day variability in dissolved oxygen concentrations and pH from September through the end of the monitoring period. For Upper Klamath Lake, seasonal (late July through early August) lows of dissolved oxygen concentrations and saturation were coincident with a seasonal low of pH values and seasonal highs of ammonia and orthophosphate concentrations, specific conductance values, and water temperatures. Patterns in these parameters, excluding water temperature, were associated with bloom dynamics of the cyanobacterium (blue-green alga) Aphanizomenonflos-aquae in Upper Klamath Lake. In Upper Klamath Lake, water temperature in excess of 28 degrees Celsius (a high stress threshold for Upper Klamath Lake suckers) was recorded only once at one site during the field season. Large areas of Upper Klamath Lake had periods of dissolved oxygen concentration of less than 4 milligrams per liter and pH value greater than 9.7, but these conditions were not persistent throughout days at most sites. Dissolved oxygen concentrations in Upper Klamath Lake on time scales of days and months appeared to be influenced, in part, by bathymetry and prevailing current flow patterns. Diel patterns of water column stratification were evident, even at the deepest sites. This diel pattern of stratification was attributable to diel wind speed patterns and the shallow nature of most of Upper Klamath Lake. Timing of the daily extreme values of dissolved oxygen concentration, pH, and water temperature was less distinct with increased water column depth. Chlorophyll a concentrations varied spatially and temporally throughout Upper Klamath Lake. Location greatly affected algal concentrations, in turn affecting nutrient and dissolved oxygen concentrations—some of the highest chlorophyll a concentrations were associated with the lowest dissolved oxygen concentrations and the highest un-ionized ammonia concentrations. The occurrence of the low dissolved oxygen and high un-ionized ammonia concentrations coincided with a decline in algae resulting from cell death, as rn.easu.red by concentrations of chlorophyll a. Dissolved oxygen production, rates in. experim.en.ts were as high as 1.47 milligrams of oxygen per liter per hour, and consumption rates were as much as -0.73 milligrams of oxygen per liter per hour. Dissolved oxygen, consumption rates measured in. this study were comparable to those measured in a 2002 Upper Klamath Lake study, and a higher rate of dissolved oxygen consumption was recorded in. dark bottles positioned higher in the water column. Data, though, inconclusive, indicated that a decreasing trend of dissolved oxygen productivity through July could have contributed to the decreasing dissolved oxygen concentrations and percent saturation recorded in Upper Klamath Lake during this time. Phytoplankton self-shading was evident from, a general inverse relation between depth of photic zone and chlorophyll a concentrations. This shading caused net dissolved oxygen consumption during daylight hours in lower parts of the water column that would otherwise have been in the photic zone. Meteorological data collected in and around Upper Klamath Lake showed that winds were likely to come from a broad range of westerly directions in the northern one-third of the lake, but tended to come from a narrow range of northwesterly directions over the main body of the lake farther south. Title: Water quality conditions in Upper Klamath and Agency Lakes, Oregon, 2005 Author: Hoilman, Gene R Year: 2008 Agency Lakes. Oregon. 2005 M.Wood By Gene R. Hoilman, Mary K. Lindenberg, and Tamara Abstract During June-October 2005, water quality data were collected from Upper Klamath and Agency Lakes In Oregon, and meteorological data were collected around and within Upper Klamath Lake. Data recorded at two continuous water quality monitors In Agency Lake showed similar temperature patterns throughout the field season, but data recorded at the northern site showed more day-to-day variability for dissolved oxygen concentration and saturation after late June and more day-to-day variability for pH and specific conductance values after mid-July. Data recorded from the northern and southern parts of Agency Lake showed more comparable day-to-day variability in dissolved oxygen concentrations and pH from September through the end of the monitoring period. For Upper Klamath Lake, seasonal (late July through early August) lows of dissolved oxygen concentrations and saturation were coincident with a seasonal low of pH values and seasonal highs of ammonia and orthophosphate concentrations, specific conductance values, and water temperatures. Patterns in these parameters, excluding water temperature, were associated with bloom dynamics of the cyanobacterium (blue-green alga) Aphanizomenonflos-aquae in Upper Klamath Lake. In Upper Klamath Lake, water temperature in excess of 28 degrees Celsius (a high stress threshold for Upper Klamath Lake suckers) was recorded only once at one site during the field season. Large areas of Upper Klamath Lake had periods of dissolved oxygen concentration of less than 4 milligrams per liter and pH value greater than 9.7, but these conditions were not persistent throughout days at most sites. Dissolved oxygen concentrations in Upper Klamath Lake on time scales of days and months appeared to be influenced, in part, by bathymetry and prevailing current flow patterns. Diel patterns of water column stratification were evident, even at the deepest sites. This diel pattern of stratification was attributable to diel wind speed patterns and the shallow nature of most of Upper Klamath Lake. Timing of the daily extreme values of dissolved oxygen concentration, pH, and water temperature was less distinct with increased water column depth. Chlorophyll a concentrations varied spatially and temporally throughout Upper Klamath Lake. Location greatly affected algal concentrations, in turn affecting nutrient and dissolved oxygen concentrations—some of the highest chlorophyll a concentrations were associated with the lowest dissolved oxygen concentrations and the highest un-ionized ammonia concentrations. The occurrence of the low dissolved oxygen and high un-ionized ammonia concentrations coincided with a decline in algae resulting from cell death, as rn.easu.red by concentrations of chlorophyll a. Dissolved oxygen production, rates in. experim.en.ts were as high as 1.47 milligrams of oxygen per liter per hour, and consumption rates were as much as -0.73 milligrams of oxygen per liter per hour. Dissolved oxygen, consumption rates measured in. this study were comparable to those measured in a 2002 Upper Klamath Lake study, and a higher rate of dissolved oxygen consumption was recorded in. dark bottles positioned higher in the water column. Data, though, inconclusive, indicated that a decreasing trend of dissolved oxygen productivity through July could have contributed to the decreasing dissolved oxygen concentrations and percent saturation recorded in Upper Klamath Lake during this time. Phytoplankton self-shading was evident from, a general inverse relation between depth of photic zone and chlorophyll a concentrations. This shading caused net dissolved oxygen consumption during daylight hours in lower parts of the water column that would otherwise have been in the photic zone. Meteorological data collected in and around Upper Klamath Lake showed that winds were likely to come from a broad range of westerly directions in the northern one-third of the lake, but tended to come from a narrow range of northwesterly directions over the main body of the lake farther south.

1597. [Image] Annual project history: Klamath Project, Oregon-California, 1957


	INTRODUCTION AND GENERAL General Description of the Project Location. The Klamath Project is in the Upper Klamath River Basin, east of the Cascade Range. It is located in Klamath County, Oregon, and ...
	Citation Citation Citation Abstract Copy Title: Annual project history: Klamath Project, Oregon-California, 1957 Author: United States. Bureau of Reclamation Year: 1957, 2008, 2006 INTRODUCTION AND GENERAL General Description of the Project Location. The Klamath Project is in the Upper Klamath River Basin, east of the Cascade Range. It is located in Klamath County, Oregon, and in Modoc and Siskiyou Counties of California. Project headquarters is located at the principal city of Klamath Falls, Oregon, which has a population of about 35>700, including suburbs. Smaller towns on the project in Oregon are Merrill, Malin, and Bonanza. The town of Tulelake, California, was established in 1931 near the center of the Tule Lake Division. Climate. The mean temperature for the wannest month is 630 F. The coldest month has mean temperature of 29? F. Summer nights are cool. The annual rainfall is about 13 inches, of which about 3?-inches fall during the growing season of 90 to 130 days. Topography, soils, and crops. The project area is about ^-,100 feet elevation above sea level. The surface topography is generally smooth and flat for the large areas of lake bottom, and gently sloping on the higher lands. Peat and muck soils are common in the recent lake bottoms. Soils vary from sandy loam to clay on other parts of the project. The principal crops grown are alfalfa, malting and feed barley, potatoes, clover seed, and irrigated pasture and other forage. Stock raising is an important enterprise. Industry and transportation. Farming and lumbering each provide the major portion of the economy of the Basin. Three major railroad lines, one major highway and many secondary highways, and two airlines serve the project area. Plan and purpose. The project serves 211,000 acres. The water supply is provided by two main water courses, Klamath River and Lost River and their tributaries. Besides storing, diverting, and distributing water for irrigation, project facilities have reclaimed by drainage large areas formerly inundated by Lower Klamath and Tule Lakes* Flood waters of Lost River, which terminates in Tule Lake, are diverted to the Klamath River through the Lost River Diversion Channel. This channel is also used to carry irrigation water in the opposite direction in the summertime. Another principal function of the project is water-level control for the Tule Lake and Lower Klamath Lake National Wildlife Refuges. Upper Klamath Lake on the Klamath River is the principal storage reservoir, having an active capacity of 52U,800 acre-feet. It is controlled by Link River Dam constructed, maintained, and operated INTRODUCTION AND GENERAL (Continued) General Description of the Project (Cont.) by The California Oregon Power Company under an agreement with the project whereby irrigation requirements and rights are protected. The Main, Lower Klamath, and Tule Lake Divisions are served from this source, Gerber Reservoir on Miller Creek and Clear Lake Reservoir on Lost River provide flood control for the Tule Lake Division and an irrigation supply for the Langell Valley Division. Their active storage capacities are 9^300 acre-feet and 513300 acre-feet, respectively. Federally-financed project works also include the diversion, distribution, and drainage systems for the Main and Tule Lake Divisions; the diversion dam and main canals for the Langell Valley Division; and drainage outlets for the Lower Klamath and Tule Lake Divisions. Title: Annual project history: Klamath Project, Oregon-California, 1957 Author: United States. Bureau of Reclamation Year: 1957, 2008, 2006 INTRODUCTION AND GENERAL General Description of the Project Location. The Klamath Project is in the Upper Klamath River Basin, east of the Cascade Range. It is located in Klamath County, Oregon, and in Modoc and Siskiyou Counties of California. Project headquarters is located at the principal city of Klamath Falls, Oregon, which has a population of about 35>700, including suburbs. Smaller towns on the project in Oregon are Merrill, Malin, and Bonanza. The town of Tulelake, California, was established in 1931 near the center of the Tule Lake Division. Climate. The mean temperature for the wannest month is 630 F. The coldest month has mean temperature of 29? F. Summer nights are cool. The annual rainfall is about 13 inches, of which about 3?-inches fall during the growing season of 90 to 130 days. Topography, soils, and crops. The project area is about ^-,100 feet elevation above sea level. The surface topography is generally smooth and flat for the large areas of lake bottom, and gently sloping on the higher lands. Peat and muck soils are common in the recent lake bottoms. Soils vary from sandy loam to clay on other parts of the project. The principal crops grown are alfalfa, malting and feed barley, potatoes, clover seed, and irrigated pasture and other forage. Stock raising is an important enterprise. Industry and transportation. Farming and lumbering each provide the major portion of the economy of the Basin. Three major railroad lines, one major highway and many secondary highways, and two airlines serve the project area. Plan and purpose. The project serves 211,000 acres. The water supply is provided by two main water courses, Klamath River and Lost River and their tributaries. Besides storing, diverting, and distributing water for irrigation, project facilities have reclaimed by drainage large areas formerly inundated by Lower Klamath and Tule Lakes* Flood waters of Lost River, which terminates in Tule Lake, are diverted to the Klamath River through the Lost River Diversion Channel. This channel is also used to carry irrigation water in the opposite direction in the summertime. Another principal function of the project is water-level control for the Tule Lake and Lower Klamath Lake National Wildlife Refuges. Upper Klamath Lake on the Klamath River is the principal storage reservoir, having an active capacity of 52U,800 acre-feet. It is controlled by Link River Dam constructed, maintained, and operated INTRODUCTION AND GENERAL (Continued) General Description of the Project (Cont.) by The California Oregon Power Company under an agreement with the project whereby irrigation requirements and rights are protected. The Main, Lower Klamath, and Tule Lake Divisions are served from this source, Gerber Reservoir on Miller Creek and Clear Lake Reservoir on Lost River provide flood control for the Tule Lake Division and an irrigation supply for the Langell Valley Division. Their active storage capacities are 9^300 acre-feet and 513300 acre-feet, respectively. Federally-financed project works also include the diversion, distribution, and drainage systems for the Main and Tule Lake Divisions; the diversion dam and main canals for the Langell Valley Division; and drainage outlets for the Lower Klamath and Tule Lake Divisions.

1598. [Image] Final report, evaluation of pond rearing of chinook salmon, project (5.12), Modification no. 1


	Abstract: Totals of 37,655 and 31,807 adipose-fin clipped, coded-wire tagged (Ad+CWT) 1990 brood year (BY) fall chinook salmon were released from ponds on Indian and Elk creeks, respectively, in 1991. ...
	Citation Citation Citation Abstract Copy Title: Final report, evaluation of pond rearing of chinook salmon, project (5.12), Modification no. 1 Author: Pisano, Mark S Year: 1993, 2005 Abstract: Totals of 37,655 and 31,807 adipose-fin clipped, coded-wire tagged (Ad+CWT) 1990 brood year (BY) fall chinook salmon were released from ponds on Indian and Elk creeks, respectively, in 1991. Numbers of fish in both ponds were inventoried and mark quality was checked shortly before the fish were released. An additional 40,078 and 41,272 1991 BY chinook salmon were Ad+CWT and transferred to Bluff Creek and Indian Creek ponds, respectively in spring JL992. These fish will be released in October 1992. Title: Final report, evaluation of pond rearing of chinook salmon, project (5.12), Modification no. 1 Author: Pisano, Mark S Year: 1993, 2005 Abstract: Totals of 37,655 and 31,807 adipose-fin clipped, coded-wire tagged (Ad+CWT) 1990 brood year (BY) fall chinook salmon were released from ponds on Indian and Elk creeks, respectively, in 1991. Numbers of fish in both ponds were inventoried and mark quality was checked shortly before the fish were released. An additional 40,078 and 41,272 1991 BY chinook salmon were Ad+CWT and transferred to Bluff Creek and Indian Creek ponds, respectively in spring JL992. These fish will be released in October 1992.

1599. [Image] Water temperature monitoring of the Klamath River mainstem: final report


	WATER TEMPERATURE MONITORING KLAMATH RIVER MAINSTEM ABSTRACT This report summarizes the water temperature data collected by the Karuk Tribe of California (Karuk Tribe) from July 1993 to September 1997 ...
	Citation Citation Citation Abstract Copy Title: Water temperature monitoring of the Klamath River mainstem: final report Author: Karuk Tribe of California Year: 1999, 2005 WATER TEMPERATURE MONITORING KLAMATH RIVER MAINSTEM ABSTRACT This report summarizes the water temperature data collected by the Karuk Tribe of California (Karuk Tribe) from July 1993 to September 1997 at thirteen locations along the Klamath River from Upper Klamath Lake to the mouth of the Klamath River at the Pacific Ocean. This report describes the water temperature monitoring system designed by the Karuk Tribe, the data checks that were performed, and a summary of the water temperature data results. The Karuk Tribe began this study in part in response to the Klamath River Basin Fisheries Task Force stated objective to monitor water temperature conditions above, within, and below existing water projects along the Klamath River. With help from the California Department of Fish and Game, PacifiCorp, and the Klamath National Forest, this project was expanded from six to thirteen original monitoring sites in 1993. Water temperature data were collected by Ryan TempMentor? instruments typically on an hourly time interval. The data was checked for accuracy by consultants and reduced for this report to mean daily water temperature values each year on a monthly basis in US Geological Survey tabular format. Mean value data were entered into a Microsoft Access relational database for use on an IBM compatible computer. Although the period of record for the Klamath River water temperature data stretches over 5 years, several gaps in data inhibit detailed analysis. The analysis presented, illustrates when the minimum and maximum preferred temperature ranges for salmonids are exceeded. In addition, preliminary temperature trend shows that in August water temperature values below Iron Gate Dam were lower than other monitoring stations further downstream. Conversely, water temperature values in October are warmer below Iron Gate than in the unregulated reaches of the Klamath River downstream. Given this information, it appears that releases from Iron Gate Dam do influence the natural water temperature balance in the Klamath River. To more accurately determine the extent of reservoir releases on the natural thermal environment, additional water temperature measurements need to be collected. Title: Water temperature monitoring of the Klamath River mainstem: final report Author: Karuk Tribe of California Year: 1999, 2005 WATER TEMPERATURE MONITORING KLAMATH RIVER MAINSTEM ABSTRACT This report summarizes the water temperature data collected by the Karuk Tribe of California (Karuk Tribe) from July 1993 to September 1997 at thirteen locations along the Klamath River from Upper Klamath Lake to the mouth of the Klamath River at the Pacific Ocean. This report describes the water temperature monitoring system designed by the Karuk Tribe, the data checks that were performed, and a summary of the water temperature data results. The Karuk Tribe began this study in part in response to the Klamath River Basin Fisheries Task Force stated objective to monitor water temperature conditions above, within, and below existing water projects along the Klamath River. With help from the California Department of Fish and Game, PacifiCorp, and the Klamath National Forest, this project was expanded from six to thirteen original monitoring sites in 1993. Water temperature data were collected by Ryan TempMentor? instruments typically on an hourly time interval. The data was checked for accuracy by consultants and reduced for this report to mean daily water temperature values each year on a monthly basis in US Geological Survey tabular format. Mean value data were entered into a Microsoft Access relational database for use on an IBM compatible computer. Although the period of record for the Klamath River water temperature data stretches over 5 years, several gaps in data inhibit detailed analysis. The analysis presented, illustrates when the minimum and maximum preferred temperature ranges for salmonids are exceeded. In addition, preliminary temperature trend shows that in August water temperature values below Iron Gate Dam were lower than other monitoring stations further downstream. Conversely, water temperature values in October are warmer below Iron Gate than in the unregulated reaches of the Klamath River downstream. Given this information, it appears that releases from Iron Gate Dam do influence the natural water temperature balance in the Klamath River. To more accurately determine the extent of reservoir releases on the natural thermal environment, additional water temperature measurements need to be collected.

1600. [Image] Administrative history: Crater Lake National Park, Oregon [volume 1]


	2 v.: ill., maps; "NPS D-71 March 1988" - [end of both volumes]; Includes bibliographical references
	Citation Citation Citation Abstract Copy Title: Administrative history: Crater Lake National Park, Oregon [volume 1] Author: Harlan D. Unrau Year: 1988, 2009, 2010 2 v.: ill., maps; "NPS D-71 March 1988" - [end of both volumes]; Includes bibliographical references Title: Administrative history: Crater Lake National Park, Oregon [volume 1] Author: Harlan D. Unrau Year: 1988, 2009, 2010 2 v.: ill., maps; "NPS D-71 March 1988" - [end of both volumes]; Includes bibliographical references

Limit your search

Material Types

Subject

Author

Pivot Field

Database

Search

Search Results

1501. [Image] An Act to Authorize the Bureau of Reclamation to Conduct Certain Feasibility Studies to Augment Water Supplies for the Klamath Project, Oregon and California, and for Other Purposes

1502. [Image] The Water Report - Critical habitat, bull trout and politics

1503. [Image] The geology and petrography of Crater lake national park

1504. [Image] Klamath River Basin Compact between the states of Oregon and California

1505. [Image] Work of the Reclamation service in Washington and Oregon

1506. [Image] Integrated land management on Tule Lake Wildlife Refuge: an alternative management strategy developed by the Integrated Land Management Working Group: promoting productive wetland habitats and sustainable agriculture on Tule Lake National Wildlife Refuge

1507. [Image] Geothermal Steam Act of 1970 and Regulations on the Leasing of Geothermal Resources

1508. [Image] SFR0028

1509. [Image] Integrated scientific assessment for ecosystem management in the interior Columbia Basin and portions of the Klamath and Great Basins

1510. [Image] Recent paleolimnology of Upper Klamath Lake, Oregon

1511. [Image] Seeking refuge: making space for migratory waterfowl and wetlands along the Pacific Flyway

1512. [Image] Lakeview proposed resource management plan and final environmental impact statement [volume 1]

1513. [Image] The South Portal Project : creating a sense of arrival

1514. [Image] Klamath Falls Resource Area resource management plan and environmental impact statement : final : Volume 1

1515. [Image] Evaluation of site specific restoration projects for the entire Klamath River basin

1516. [Image] Crater Lake limnological studies: final report

1517. [Image] Region II Klamath Project annual history, 1945

1518. [Image] Federal Register - Endangered and Threatened Wildlife and Plants; Notice of 90-Day Finding on a Petition to Delist the Lost River Sucker and Shortnose Sucker

1519. [Image] Forest conditions in the Cascade Range Forest Reserve, Oregon

1520. [Image] The Water Report. Klamath Fishery Science: Controversy in the Klamath River Basin

1521. [Image] Soil survey of Crater Lake National Park, Oregon

1522. [Image] Trinity River Flow Evaluation: final report: a report to the Secretary , U.S. Department of the Interior

1523. [Image] Agricultural information on Klamath County irrigation

1524. [Image] Ecology of shortnose and Lost River suckers in Tule Lake National Wildlife Refuge, California : progress report, April - November 1999

1525. [Image] Summary of ongoing and planned work of the Department of the Interior related to the Klamath River Basin, March 2003

1526. [Image] IMST review of the USFWS and NMFS 2001 biological opinions on management of the Klamath Reclamation Project and related reports: a report of the Independent Multidisciplinary Science Team, Oregon Plan for Salmon and Watersheds

1527. [Image] Klamath River Basin issues and activities

1528. [Image] The Oregon conservation strategy

1529. [Image] The Water Report - The ESA, salmon, and Western water law

1530. [Image] Restoring Harmony in the Klamath Basin

1531. [Image] Ground water hydrology of four proposed project areas in the Klamath Basin, Oregon

1532. [Image] Biological assessment of Klamath Project's continuing operations on the endangered Lost River sucker and shortnose sucker

1533. [Image] Making the ESA work better: implementing the 10 point plan - and beyond

1534. [Image] Klamath Project : historic operation

1535. [Image] Nitrogen and phosphorus loading from drained wetlands adjacent to Upper Klamath and Agency Lakes, Oregon

1536. [Image] Technical assistance and the Oregon Plan for Salmon and Watersheds: a statewide assessment by the Healthy Streams Partnership

1537. [Image] Federal Register - Endangered and Threatened Wildlife and Plants; Notice of Revised 90-Day Petition Finding and Initiation of a 5-Year Status Review of the Lost River Sucker and Shortnose Sucker

1538. [Image] Agreement with Indians of Klamath Reservation, Oregon

1539. [Image] Reproductive biology and demographics of endangered Lost River and shortnose suckers in Upper Klamath Lake, Oregon

1540. [Image] Farming practices and water quality in the Upper Klamath Basin : final report to the California State Water Resources Control Board : 205j program

1541. [Image] Crater Lake market assessment

1542. [Image] The Chemical and biological impact of Klamath Marsh on the Williamson River, Oregon

1543. [Image] Soils of the Klamath Indian Reservation; interim report, June 11, 1958

1544. [Image] Water-quality data from 2002 to 2003 and analysis of data gaps for development of total maximum daily loads in the Lower Klamath River basin, California

1545. [Image] Western water supply : hearing before the Committee on Energy and Natural Resources, United States Senate, One Hundred Eighth Congress, second session, to receive testimony regarding water supply issues in the arid West, March 9, 2004

1546. [Image] Handbook for developing watershed plans to restore and protect our waters

1547. [Image] Distribution and biology of suckers in Lower Klamath reservoirs : 1999 final report

1548. [Image] Natural history and ecology of larval Lost River suckers and larval shortnose suckers in the Williamson River-Upper Klamath Lake System

1549. [Image] Klamath Project : hearing before the Subcommittee on Water and Power of the Committee on Energy and Natural Resources, United States Senate, One Hundred Seventh Congress, first session to discuss Klamath Project operations and implementation of Public Law 106-498, March 21, 2001

1550. [Image] Crater Lake National Park oral history series, Emmett Blanchfield

1551. [Image] An assessment of ecosystem components in the interior Columbia Basin and portions of the Klamath and Great Basins [volume 2]

1552. [Image] Water management and endangered species issues in the Klamath Basin : oversight field hearing before the Committee on Resources, U.S. House of Representatives, One Hundred Seventh Congress, first session, June 16, 2001 in Klamath Falls, Oregon

1553. [Image] Soil survey of Klamath County, Oregon, southern part

1554. [Image] Anomalies of larval and juvenile shortnose and Lost River suckers in Upper Klamath Lake, Oregon

1555. [Image] Hydrogeology and paleohydrology in the Williamson River basin, Klamath County, Oregon

1556. [Image] Report of 1994 Workshop on the Correlation of Marine and Terrestrial Records of Climate Changes in the Western United States

1558. [Image] An examination of the Klamath Basin crisis : restructuring the discourse within an identity-based framework

1559. [Image] Annual project history and O. & M. report of the Klamath Project, Oregon-California, 1918

1560. [Image] Annual report of the Klamath Project, Oregon-California, 1917

1561. [Image] The Bull trout (salvelinus confluentus) population within Crater Lake National Park: summarized information relating to its conservation and perpetuation

1562. [Image] Bull trout restoration and brook trout eradication at Crater Lake National Park, Oregon

1563. [Image] A framework for ecosystem management in the interior Columbia Basin and portions of the Klamath and Great Basins

1564. [Image] Bull Trout, Salvelinus Confluentus... Draft Recovery Plan, Chapter 2, Klamath River Recovery Unit...U.S. Department Of The Interior

1565. [Image] Geological limnology of Crater Lake, Oregon

1566. [Image] Geology and ground-water resources of the Swan Lake-Yonna Valleys area, Klamath County, Oregon

1567. [Image] Scientific disagreement regarding coho salmon status under the ESA

1568. [Image] Improving salmon passage: draft, the Lower Snake River juvenile salmon migration feasibility report/environmental impact statement

1569. [Image] Volcano and earthquake hazards in the Crater Lake Region, Oregon: open file report 97-487

1570. [Image] The estimation of regional secondary benefits resulting from an improvement in water quality of Upper Klamath Lake, Oregon: an interindustry approach

1571. [Image] Bull Trout, Salvelinus Confluentus... Draft Recovery Plan, Chapter 1, Introduction...