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• 6091. [Image] Nutrients in the nation's waters : too much of a good thing?

  	Includes bibliographical references (p. 22)
  	Citation × Citation Citation Abstract Copy Title: Nutrients in the nation's waters : too much of a good thing? Author: Mueller, David K. Year: 1996, 2004 Includes bibliographical references (p. 22) Title: Nutrients in the nation's waters : too much of a good thing? Author: Mueller, David K. Year: 1996, 2004 Includes bibliographical references (p. 22) Close

• 6092. [Image] Klamath River water quality and acoustic Doppler current profiler data from Link River Dam to Keno Dam, 2007

  	Klamath River Water Quality and Acoustic Doppler Current Profiler Data from Link River Dam to Keno Dam, 2007 By Annett B. Sullivan, Michael L. Deas, Jessica Asbill, Julie D. Kirshtein, Kenna Butler, Roy ...
  	Citation × Citation Citation Abstract Copy Title: Klamath River water quality and acoustic Doppler current profiler data from Link River Dam to Keno Dam, 2007 Author: Sullivan, Annett B. (Annett Brigitte), 1970- Year: 2008 Klamath River Water Quality and Acoustic Doppler Current Profiler Data from Link River Dam to Keno Dam, 2007 By Annett B. Sullivan, Michael L. Deas, Jessica Asbill, Julie D. Kirshtein, Kenna Butler, Roy E. Wellman, Marc A. Stewart, and Jennifer Vaughn Abstract In 2007, the U.S. Geological Survey, Watercourse Engineering, and Bureau of Reclamation began a project to construct and calibrate a water quality and hydrodynamic model of the 21-mile reach of the Klamath River from Link River Dam to Keno Dam. To provide a basis for this work, data collection and experimental work were planned for 2007 and 2008. This report documents sampling and analytical methods and presents data from the first year of work. To determine water velocities and discharge, a series of cross-sectional acoustic Doppler current profiler (ADCP) measurements were made on the mainstem and four canals on May 30 and September 19, 2007. Water quality was sampled weekly at five mainstem sites and five tributaries from early April through early November, 2007. Constituents reported here include field parameters (water temperature, pH, dissolved oxygen concentration, specific conductance); total nitrogen and phosphorus; particulate carbon and nitrogen; filtered orthophosphate, nitrite, nitrite plus nitrate, ammonia, organic carbon, iron, silica, and alkalinity; specific UV absorbance at 254 nm; phytoplankton and zooplankton enumeration and species identification; and bacterial abundance and morphological subgroups. The ADCP measurements conducted in good weather conditions in May showed that four major canals accounted for most changes in discharge along the mainstem on that day. Direction of velocity at measured locations was fairly homogeneous across the channel, while velocities were generally lowest near the bottom, and highest near surface, ranging from 0.0 to 0.8 ft/s. Measurements in September, made in windy conditions, raised questions about the effect of wind on flow. Most nutrient and carbon concentrations were lowest in spring, increased and remained elevated in summer, and decreased in fall. Dissolved nitrite plus nitrate and nitrite had a different seasonal cycle and were below detection or at low concentration in summer. Many nutrient and carbon concentrations were similar at the top and bottom of the water column, though ammonia and particulate carbon showed more variability in summer. Averaged over the season, particulate carbon and particulate nitrogen decreased in the downstream direction, while ammonia and orthophosphate concentrations increased in the downstream direction. At most sites, bacteria, phytoplankton, and zooplankton populations reached their maximums in summer. Large bacterial cells made up most of the bacteria biovolume, though cocci were the most numerous bacteria type. The cocci were smaller than the filter pore sizes used to separate dissolved from particulate matter in this study. Phytoplankton biovolumes were dominated by the blue-green alga Aphanizomenonflos aquae most of the sampling season, though a spring diatom bloom occurred. Phytoplankton biovolumes were generally highest at the upstream Link River and Railroad Bridge sites and decreased in the downstream direction. Zooplankton populations were dominated by copepods in early spring, and by cladocerans and rotifers in summer, with rotifers more common farther downstream. l Title: Klamath River water quality and acoustic Doppler current profiler data from Link River Dam to Keno Dam, 2007 Author: Sullivan, Annett B. (Annett Brigitte), 1970- Year: 2008 Klamath River Water Quality and Acoustic Doppler Current Profiler Data from Link River Dam to Keno Dam, 2007 By Annett B. Sullivan, Michael L. Deas, Jessica Asbill, Julie D. Kirshtein, Kenna Butler, Roy E. Wellman, Marc A. Stewart, and Jennifer Vaughn Abstract In 2007, the U.S. Geological Survey, Watercourse Engineering, and Bureau of Reclamation began a project to construct and calibrate a water quality and hydrodynamic model of the 21-mile reach of the Klamath River from Link River Dam to Keno Dam. To provide a basis for this work, data collection and experimental work were planned for 2007 and 2008. This report documents sampling and analytical methods and presents data from the first year of work. To determine water velocities and discharge, a series of cross-sectional acoustic Doppler current profiler (ADCP) measurements were made on the mainstem and four canals on May 30 and September 19, 2007. Water quality was sampled weekly at five mainstem sites and five tributaries from early April through early November, 2007. Constituents reported here include field parameters (water temperature, pH, dissolved oxygen concentration, specific conductance); total nitrogen and phosphorus; particulate carbon and nitrogen; filtered orthophosphate, nitrite, nitrite plus nitrate, ammonia, organic carbon, iron, silica, and alkalinity; specific UV absorbance at 254 nm; phytoplankton and zooplankton enumeration and species identification; and bacterial abundance and morphological subgroups. The ADCP measurements conducted in good weather conditions in May showed that four major canals accounted for most changes in discharge along the mainstem on that day. Direction of velocity at measured locations was fairly homogeneous across the channel, while velocities were generally lowest near the bottom, and highest near surface, ranging from 0.0 to 0.8 ft/s. Measurements in September, made in windy conditions, raised questions about the effect of wind on flow. Most nutrient and carbon concentrations were lowest in spring, increased and remained elevated in summer, and decreased in fall. Dissolved nitrite plus nitrate and nitrite had a different seasonal cycle and were below detection or at low concentration in summer. Many nutrient and carbon concentrations were similar at the top and bottom of the water column, though ammonia and particulate carbon showed more variability in summer. Averaged over the season, particulate carbon and particulate nitrogen decreased in the downstream direction, while ammonia and orthophosphate concentrations increased in the downstream direction. At most sites, bacteria, phytoplankton, and zooplankton populations reached their maximums in summer. Large bacterial cells made up most of the bacteria biovolume, though cocci were the most numerous bacteria type. The cocci were smaller than the filter pore sizes used to separate dissolved from particulate matter in this study. Phytoplankton biovolumes were dominated by the blue-green alga Aphanizomenonflos aquae most of the sampling season, though a spring diatom bloom occurred. Phytoplankton biovolumes were generally highest at the upstream Link River and Railroad Bridge sites and decreased in the downstream direction. Zooplankton populations were dominated by copepods in early spring, and by cladocerans and rotifers in summer, with rotifers more common farther downstream. l Close

• 6093. [Image] Water resources data. Oregon. Water Year 2002

  	PREFACEThe annual Oregon hydrologic data report is one of a series of annual reports that document hydrologic data gathered from the U.S. Geological Survey's surface- and ground-water data-collection networks ...
  	Citation × Citation Citation Abstract Copy Title: Water resources data. Oregon. Water Year 2002 Author: Geological Survey (U.S.). Water Resources Division Year: 2002, 2004 PREFACEThe annual Oregon hydrologic data report is one of a series of annual reports that document hydrologic data gathered from the U.S. Geological Survey's surface- and ground-water data-collection networks in each State, Puerto Rico, and the Trust Territories. These records of streamflow, ground-water levels, and quality of water provide the hydrologic information needed by State, local and Federal agencies, and the private sector for developing and managing our Nation's land and water resources.The report is the culmination of a concerted effort by dedicated personnel of the U.S. Geological Survey who collected, compiled, analyzed, verified, and organized the data, and who edited and assembled the reports. In addition to the authors, who had primary responsibility for assuring that the information contained herein is accurate, complete, and adheres to Geological Survey policy and established guidelines, the following individuals contributed significantly to the collection, processing, and tabulation of the data: Title: Water resources data. Oregon. Water Year 2002 Author: Geological Survey (U.S.). Water Resources Division Year: 2002, 2004 PREFACEThe annual Oregon hydrologic data report is one of a series of annual reports that document hydrologic data gathered from the U.S. Geological Survey's surface- and ground-water data-collection networks in each State, Puerto Rico, and the Trust Territories. These records of streamflow, ground-water levels, and quality of water provide the hydrologic information needed by State, local and Federal agencies, and the private sector for developing and managing our Nation's land and water resources.The report is the culmination of a concerted effort by dedicated personnel of the U.S. Geological Survey who collected, compiled, analyzed, verified, and organized the data, and who edited and assembled the reports. In addition to the authors, who had primary responsibility for assuring that the information contained herein is accurate, complete, and adheres to Geological Survey policy and established guidelines, the following individuals contributed significantly to the collection, processing, and tabulation of the data: Close

• 6094. [Image] Modeling hydrodynamics and heat transport in upper Klamath Lake, Oregon, and implications for water quality

  	Title from PDF title screen (viewed on June 13, 2008); Includes bibliographical references;
  	Citation × Citation Citation Abstract Copy Title: Modeling hydrodynamics and heat transport in upper Klamath Lake, Oregon, and implications for water quality Author: Wood, Tamara M.; Cheng, Ralph T.; Gartner, Jeffrey W.; Hoilman, Gene R.; Lindenberg, Mary K.; Wellman, Roy E. Year: 2008 Title from PDF title screen (viewed on June 13, 2008); Includes bibliographical references; Title: Modeling hydrodynamics and heat transport in upper Klamath Lake, Oregon, and implications for water quality Author: Wood, Tamara M.; Cheng, Ralph T.; Gartner, Jeffrey W.; Hoilman, Gene R.; Lindenberg, Mary K.; Wellman, Roy E. Year: 2008 Title from PDF title screen (viewed on June 13, 2008); Includes bibliographical references; Close

• 6095. [Image] Determining surface water availability in Oregon : open file report SW 02-002

  	Determining Surface Water Availability in Oregon By Richard M. Cooper, PE Abstract The Oregon Water Resources Department (Department or OWRD) limits appropriation from Oregon streams to assure new applicants ...
  	Citation × Citation Citation Abstract Copy Title: Determining surface water availability in Oregon : open file report SW 02-002 Author: Oregon. Water Resources Dept. Year: 2002, 2005 Determining Surface Water Availability in Oregon By Richard M. Cooper, PE Abstract The Oregon Water Resources Department (Department or OWRD) limits appropriation from Oregon streams to assure new applicants use of surface water a reasonable amount of time and to minimize regulatory conflict. The standards for new appropriation of water are: (1) consumptive use from allocations for out-of-stream uses can total no more than the 80-percent ex-ceedance natural stream flow, and (2) allocations for in-stream flows can be no more than the 50-percent exceedance natural stream flow. OWRD has created and maintains a database of the amount of surface water available for appropriation for most waters in the state. This database is used to evaluate applications for new uses of water. Water availability (WA) is obtained from natural stream flow (QNSF) by subtracting existing storage (ST), out-of-stream consumptive uses (CU) and in-stream demands (IS). WA = QN -ST-CU-IS Ideally, water availability would be calculated for every watershed above a point of diversion or in-stream demand. Practically, the number of watersheds must be limited. The watersheds selected for analysis are called Water Availability Basins (WABs). Stream flow can be highly variable, and it is useful to characterize it in some way, usually by a statistic, e.g., a monthly or annual mean. For water availability, it is important to know how often water is available. The appropriate statistic in this case is exceedance stream flow. This statistic tells us how often to expect a given rate of stream flow to occur. Exceedance stream flows are determined directly from gage records, or for ungaged streams, by estimation through modeling. When determined from gage records, the exceedance flows must be corrected to a common base period, and then, to natural stream flow. When determined through modeling, the exceedance flows are estimated from statistical models that relate watershed characteristics to natural stream flow. The models are derived by multiple linear regression. Storage is water retained in a reservoir. It is debited from water availability when the water is stored. It diminishes availability both upstream and downstream of the point of diversion. Consumptive use is divided into three major categories: irrigation, municipal, and all others e.g., domestic, livestock. These uses are less than 100 percent consumptive. It is assumed the non-consumed part of a diversion is returned to the stream from which it was diverted. Consumptive use from irrigation is from estimates made by the US Geological Survey (Portland). Consumption from other uses is based on the associated water rights. In these cases, consumptive use is obtained by multiplying the maximum diversion rate allowed for the water right by a consumptive use coefficient. Consumptive use diminishes availability both upstream and downstream of the point of diversion. There are two types of in-stream demands: in-stream water rights and scenic waterway flows. In-stream demands diminish availability upstream only. Because they are non-consumptive, they do not diminish stream flow downstream as do consumptive uses. Water availability has been calculated for over 2500 WABs. In general, the calculation of water availability at one WAB cannot be considered in isolation from other WABs in the same stream system. For water to be available at any given upstream point, it must be available at all points of calculation downstream. Title: Determining surface water availability in Oregon : open file report SW 02-002 Author: Oregon. Water Resources Dept. Year: 2002, 2005 Determining Surface Water Availability in Oregon By Richard M. Cooper, PE Abstract The Oregon Water Resources Department (Department or OWRD) limits appropriation from Oregon streams to assure new applicants use of surface water a reasonable amount of time and to minimize regulatory conflict. The standards for new appropriation of water are: (1) consumptive use from allocations for out-of-stream uses can total no more than the 80-percent ex-ceedance natural stream flow, and (2) allocations for in-stream flows can be no more than the 50-percent exceedance natural stream flow. OWRD has created and maintains a database of the amount of surface water available for appropriation for most waters in the state. This database is used to evaluate applications for new uses of water. Water availability (WA) is obtained from natural stream flow (QNSF) by subtracting existing storage (ST), out-of-stream consumptive uses (CU) and in-stream demands (IS). WA = QN -ST-CU-IS Ideally, water availability would be calculated for every watershed above a point of diversion or in-stream demand. Practically, the number of watersheds must be limited. The watersheds selected for analysis are called Water Availability Basins (WABs). Stream flow can be highly variable, and it is useful to characterize it in some way, usually by a statistic, e.g., a monthly or annual mean. For water availability, it is important to know how often water is available. The appropriate statistic in this case is exceedance stream flow. This statistic tells us how often to expect a given rate of stream flow to occur. Exceedance stream flows are determined directly from gage records, or for ungaged streams, by estimation through modeling. When determined from gage records, the exceedance flows must be corrected to a common base period, and then, to natural stream flow. When determined through modeling, the exceedance flows are estimated from statistical models that relate watershed characteristics to natural stream flow. The models are derived by multiple linear regression. Storage is water retained in a reservoir. It is debited from water availability when the water is stored. It diminishes availability both upstream and downstream of the point of diversion. Consumptive use is divided into three major categories: irrigation, municipal, and all others e.g., domestic, livestock. These uses are less than 100 percent consumptive. It is assumed the non-consumed part of a diversion is returned to the stream from which it was diverted. Consumptive use from irrigation is from estimates made by the US Geological Survey (Portland). Consumption from other uses is based on the associated water rights. In these cases, consumptive use is obtained by multiplying the maximum diversion rate allowed for the water right by a consumptive use coefficient. Consumptive use diminishes availability both upstream and downstream of the point of diversion. There are two types of in-stream demands: in-stream water rights and scenic waterway flows. In-stream demands diminish availability upstream only. Because they are non-consumptive, they do not diminish stream flow downstream as do consumptive uses. Water availability has been calculated for over 2500 WABs. In general, the calculation of water availability at one WAB cannot be considered in isolation from other WABs in the same stream system. For water to be available at any given upstream point, it must be available at all points of calculation downstream. Close

• 6096. [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. Close

• 6097. [Image] Water availability for Oregon's rivers and streams: Volume 2; Technical guide and appendixes

  	Title from cover; "May 1991"
  	Citation × Citation Citation Abstract Copy Title: Water availability for Oregon's rivers and streams: Volume 2; Technical guide and appendixes Author: Robison, E. George Year: 1991, 2004 Title from cover; "May 1991" Title: Water availability for Oregon's rivers and streams: Volume 2; Technical guide and appendixes Author: Robison, E. George Year: 1991, 2004 Title from cover; "May 1991" Close

• 6098. [Image] Effects of the drought on small business and agriculture : hearings before the Select Committee on Small Business, United States Senate, Ninety-fifth Congress, first session ... Klamath Falls, Oreg., August 16, 1977, Burns, Oreg., August 17, 1977

  	CONTENTS Statement of?©ag!, Anklin, William 2620 115 Barnett, Hon. Leo, Judge, Gilliam County, Oreg 2620 196 Chapman, James, president, Klamath Cattlemen's Association, Inc., Klamath Falls, Oreg ...
  	Citation × Citation Citation Abstract Copy Title: Effects of the drought on small business and agriculture : hearings before the Select Committee on Small Business, United States Senate, Ninety-fifth Congress, first session ... Klamath Falls, Oreg., August 16, 1977, Burns, Oreg., August 17, 1977 Author: United States. Congress. Senate. Select Committee on Small Business Year: 1977, 2005, 2004 CONTENTS Statement of?©ag!, Anklin, William 2620 115 Barnett, Hon. Leo, Judge, Gilliam County, Oreg 2620 196 Chapman, James, president, Klamath Cattlemen's Association, Inc., Klamath Falls, Oreg 269 112 Cockram, Fred J., president, Oregon Dairymen's Association 2620 116 Cody, Jim, District Director, Farmers Home Administration, Port land, Oreg 2620 184 Eisgruber, Ludwig M., professor and head of the Department of Agri cultural and Resource Economics, School of Agriculture, Oregon State University 2620 118 Flitcraft, Hon. George C, Mayor, city of Klamath Falls, Klamath Falls, Oreg 2620 1 Fujii, Howard, manager, Public Affairs, Oregon Farm Bureau Fed eration 2620 170 Gift, Lloyd 2620 110 Goertzen, Victor, Assistant District Director, Management Assistance, Boise District Office, U.S. Small Business Administration 2620 189 Graham, Jack, coordinator, Agricultural Drought Office, State of Oregon 2620 174 Hagelstein, Fred, assistant director, Oregon State University Exten sion Service, Corvallis, Oreg 2620 39 Hawkins, Bert, president, Oregon Cattlemen's Association, Ontario, Oreg 2620 5 Hernandez, Richard, Associate Administrator for Operation- U.S. Small Business Administration, accompanied by J. Don Chapman, District Director, Portland District Office, SBA 2620 74 Huff, Bert, regional vice president, First National Bank of Oregon, Portland, Oreg 2620 129 Johnson, Samuel, member of the legislature, Klamath County, Oreg 2620 5 Langley, Dwight, representing Baker County Livestock Association, Baker, Oreg 2620 157 Mayer, William H., Regional Director, Federal Disaster Assistance Administration, Region 10, Seattle, Wash 2620 94 Miller, Tad, president, Oregon Wheat Growers League, Pendleton, Oreg., accompanied by Wes Grilley 2620 160 Nicholson, Mr 2620 110 Otley, Charles, past president, Oregon Cattlemen's Association 2620 196 Ross, Bill, first vice president, Oregon Cattlemen's Association 2620 146 Sehorn, Talbert D., State Executive Director, Agricultural Stabiliza tion and Conservation Service, U.S. Department of Agriculture 2620 103 Sitz, James H., president, Harney County Stockgrowers, Drewsey, Oreg 2620 197 Skinner, Bob, president, Malheur County Livestock Association 2620 151 Smith, Earl, member, State Department of Agriculture, Salem, Oreg 2620 140 Storms, Murl W., State Director, Oregon State Office, Bureau of Land Management, Portland, Oreg 2620 65 Thorne, Raymond P., Board of County Commissioners, County Commissioners Chambers, Klamath County Courthouse Annex, Klamath Falls, Oreg 2620 2 White, Hon. Dale, County Judge for Harney County, Burns, Oreg- 2620 134 Williams, Gary, representing the Oregon Wool Growers Association._ 21 Zinn, Thomas G., Wasco County Extension Agent, Oregon State Uni versity Extension Service 2620 48 (in) IV APPENDIX Statement of Edward Peile, president, Jackson County Stockmen's As- sociation 2620 201 Statement of Mike Hanley, Jordan Valley, Oreg 2620 201 Statement of Gene Officer, president, Grant County Stockgrowers Asso ciation, Canyon City, Oreg 2620 204 HEARING DATES August 16, 1977: Afternoon session 2620 1 August 17,1977: Afternoon session 2620 133 Title: Effects of the drought on small business and agriculture : hearings before the Select Committee on Small Business, United States Senate, Ninety-fifth Congress, first session ... Klamath Falls, Oreg., August 16, 1977, Burns, Oreg., August 17, 1977 Author: United States. Congress. Senate. Select Committee on Small Business Year: 1977, 2005, 2004 CONTENTS Statement of?©ag!, Anklin, William 2620 115 Barnett, Hon. Leo, Judge, Gilliam County, Oreg 2620 196 Chapman, James, president, Klamath Cattlemen's Association, Inc., Klamath Falls, Oreg 269 112 Cockram, Fred J., president, Oregon Dairymen's Association 2620 116 Cody, Jim, District Director, Farmers Home Administration, Port land, Oreg 2620 184 Eisgruber, Ludwig M., professor and head of the Department of Agri cultural and Resource Economics, School of Agriculture, Oregon State University 2620 118 Flitcraft, Hon. George C, Mayor, city of Klamath Falls, Klamath Falls, Oreg 2620 1 Fujii, Howard, manager, Public Affairs, Oregon Farm Bureau Fed eration 2620 170 Gift, Lloyd 2620 110 Goertzen, Victor, Assistant District Director, Management Assistance, Boise District Office, U.S. Small Business Administration 2620 189 Graham, Jack, coordinator, Agricultural Drought Office, State of Oregon 2620 174 Hagelstein, Fred, assistant director, Oregon State University Exten sion Service, Corvallis, Oreg 2620 39 Hawkins, Bert, president, Oregon Cattlemen's Association, Ontario, Oreg 2620 5 Hernandez, Richard, Associate Administrator for Operation- U.S. Small Business Administration, accompanied by J. Don Chapman, District Director, Portland District Office, SBA 2620 74 Huff, Bert, regional vice president, First National Bank of Oregon, Portland, Oreg 2620 129 Johnson, Samuel, member of the legislature, Klamath County, Oreg 2620 5 Langley, Dwight, representing Baker County Livestock Association, Baker, Oreg 2620 157 Mayer, William H., Regional Director, Federal Disaster Assistance Administration, Region 10, Seattle, Wash 2620 94 Miller, Tad, president, Oregon Wheat Growers League, Pendleton, Oreg., accompanied by Wes Grilley 2620 160 Nicholson, Mr 2620 110 Otley, Charles, past president, Oregon Cattlemen's Association 2620 196 Ross, Bill, first vice president, Oregon Cattlemen's Association 2620 146 Sehorn, Talbert D., State Executive Director, Agricultural Stabiliza tion and Conservation Service, U.S. Department of Agriculture 2620 103 Sitz, James H., president, Harney County Stockgrowers, Drewsey, Oreg 2620 197 Skinner, Bob, president, Malheur County Livestock Association 2620 151 Smith, Earl, member, State Department of Agriculture, Salem, Oreg 2620 140 Storms, Murl W., State Director, Oregon State Office, Bureau of Land Management, Portland, Oreg 2620 65 Thorne, Raymond P., Board of County Commissioners, County Commissioners Chambers, Klamath County Courthouse Annex, Klamath Falls, Oreg 2620 2 White, Hon. Dale, County Judge for Harney County, Burns, Oreg- 2620 134 Williams, Gary, representing the Oregon Wool Growers Association._ 21 Zinn, Thomas G., Wasco County Extension Agent, Oregon State Uni versity Extension Service 2620 48 (in) IV APPENDIX Statement of Edward Peile, president, Jackson County Stockmen's As- sociation 2620 201 Statement of Mike Hanley, Jordan Valley, Oreg 2620 201 Statement of Gene Officer, president, Grant County Stockgrowers Asso ciation, Canyon City, Oreg 2620 204 HEARING DATES August 16, 1977: Afternoon session 2620 1 August 17,1977: Afternoon session 2620 133 Close

• 6099. [Image] Proceedings of the Klamath Basin Fish & Water Management Symposium

  	ABSTRACT Two facilitated discussions were held with participants during the last two days of the Klamath Basin Fish and Water Symposium with the goal of proposing next steps that could be taken to resolve ...
  	Citation × Citation Citation Abstract Copy Title: Proceedings of the Klamath Basin Fish & Water Management Symposium Author: Klamath River Inter-Tribal Fish & Water Commission. ; Humboldt State University. Year: 2002, 2008, 2005 ABSTRACT Two facilitated discussions were held with participants during the last two days of the Klamath Basin Fish and Water Symposium with the goal of proposing next steps that could be taken to resolve the issues regarding water use and restoration in the basin. This paper is a compilation of the results from the facilitated sessions. Title: Proceedings of the Klamath Basin Fish & Water Management Symposium Author: Klamath River Inter-Tribal Fish & Water Commission. ; Humboldt State University. Year: 2002, 2008, 2005 ABSTRACT Two facilitated discussions were held with participants during the last two days of the Klamath Basin Fish and Water Symposium with the goal of proposing next steps that could be taken to resolve the issues regarding water use and restoration in the basin. This paper is a compilation of the results from the facilitated sessions. Close