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• 1591. [Article] Warner Valley Fish Investigations- Warner Suckers Progress Reports 2008

  Abstract -- The Warner sucker (Catostomus warnerensis) is endemic to the Warner Valley, an endorheic subbasin of the Great Basin in southeastern Oregon and northwestern Nevada. This species was historically ...

  Citation × Citation Citation Abstract Copy Title: Warner Valley Fish Investigations- Warner Suckers Progress Reports 2008 Abstract -- The Warner sucker (Catostomus warnerensis) is endemic to the Warner Valley, an endorheic subbasin of the Great Basin in southeastern Oregon and northwestern Nevada. This species was historically abundant and its historical range includes three permanent lakes (Hart, Crump, and Pelican), several ephemeral lakes, a network of sloughs and diversion canals, and three major tributary drainages (Honey, Deep, and Twentymile Creeks). Warner sucker abundance and distribution has declined over the past century and it was federally listed as threatened in 1985 due to habitat fragmentation and threats posed by the proliferation of piscivorous non-native game fishes (U.S. Fish and Wildlife Service 1985). The Warner Valley is a northeast-southwest trending endorheic basin which extends approximately 90 km (Figure 1). The elevation of the valley floor is approximately 1,370 m and the basin is bound by fault block escarpments, the Warner Rim on the west and Hart Mountain and Poker Jim Ridge on the east. The Warner basin was formed during the middle Tertiary and late Quaternary geologic periods as a result of volcanic and tectonic activity (Baldwin 1976). Abundant precipitation during the Pleistocene Epoch resulted in the formation of Pluvial Lake Warner (Hubbs and Miller 1948). At its maximum extent approximately 11,000 years ago, the lake reached approximately 100 m in depth and 1,300 km2 in area (Snyder et al. 1964, Weide 1975). In 2008, precipitation and snow pack were near average and Hart and Crump Lakes never filled completely. In 2007, Crump Lake water levels were very low with less than a quarter of the surface area wetted during the winter. Both lakes have been watered continuously since 1993. The Warner sucker inhabits the lakes and low gradient stream reaches of the Warner Valley. Two life history forms are present that comprise the metapopulation of Warner suckers: lake and stream morphs. The lake suckers are lacustrine adfluvial or potamodromous fish which normally spawn in the streams. However, upstream migration may be blocked by low stream flows during dry water years or by irrigation diversion dams and spawning may occur in nearshore areas of the lakes (White et al. 1990). The stream suckers inhabit and spawn in the three major tributary drainages (Honey, Deep, and Twentymile Creeks). Large lake-dwelling populations of introduced fishes in the lakes likely reduce sucker recruitment by predation on young suckers (U.S. Fish and Wildlife Service 1998). The Recovery Plan for the Threatened and Rare Native Fishes of the Warner Basin and Alkali Subbasin (U.S. Fish and Wildlife Service 1998) sets recovery criteria for delisting the species. These criteria require that (1) a self-sustaining metapopulation is distributed throughout the Twentymile, Honey, and Deep Creek (below the falls) drainages, and in Pelican, Crump, and Hart Lakes, (2) passage is restored within and among the Twentymile, Honey, and Deep Creek (below the falls) drainages so that the individual populations of Warner suckers can function as a metapopulation, and (3) no threats exist that would likely threaten the survival of the species over a significant portion of its range. In 2008, we conducted investigations in Hart and Crump Lakes to quantify the abundance and distribution of Warner suckers, to search for evidence of recent recruitment, and to estimate sucker abundance relative to nonnative fish abundance. In addition we investigated growth and movement patterns. We used Passive Integrated Transponder (PIT) tagged suckers to determine growth rates and movements, tracked radio-tagged suckers to document seasonal spawning migrations, fished a screw trap in Twelvemile Creek to monitor downstream movements, and operated a trap at the Dyke diversion dam on Twentymile Creek to monitor upstream movements. Title: Warner Valley Fish Investigations- Warner Suckers Progress Reports 2008 Abstract -- The Warner sucker (Catostomus warnerensis) is endemic to the Warner Valley, an endorheic subbasin of the Great Basin in southeastern Oregon and northwestern Nevada. This species was historically abundant and its historical range includes three permanent lakes (Hart, Crump, and Pelican), several ephemeral lakes, a network of sloughs and diversion canals, and three major tributary drainages (Honey, Deep, and Twentymile Creeks). Warner sucker abundance and distribution has declined over the past century and it was federally listed as threatened in 1985 due to habitat fragmentation and threats posed by the proliferation of piscivorous non-native game fishes (U.S. Fish and Wildlife Service 1985). The Warner Valley is a northeast-southwest trending endorheic basin which extends approximately 90 km (Figure 1). The elevation of the valley floor is approximately 1,370 m and the basin is bound by fault block escarpments, the Warner Rim on the west and Hart Mountain and Poker Jim Ridge on the east. The Warner basin was formed during the middle Tertiary and late Quaternary geologic periods as a result of volcanic and tectonic activity (Baldwin 1976). Abundant precipitation during the Pleistocene Epoch resulted in the formation of Pluvial Lake Warner (Hubbs and Miller 1948). At its maximum extent approximately 11,000 years ago, the lake reached approximately 100 m in depth and 1,300 km2 in area (Snyder et al. 1964, Weide 1975). In 2008, precipitation and snow pack were near average and Hart and Crump Lakes never filled completely. In 2007, Crump Lake water levels were very low with less than a quarter of the surface area wetted during the winter. Both lakes have been watered continuously since 1993. The Warner sucker inhabits the lakes and low gradient stream reaches of the Warner Valley. Two life history forms are present that comprise the metapopulation of Warner suckers: lake and stream morphs. The lake suckers are lacustrine adfluvial or potamodromous fish which normally spawn in the streams. However, upstream migration may be blocked by low stream flows during dry water years or by irrigation diversion dams and spawning may occur in nearshore areas of the lakes (White et al. 1990). The stream suckers inhabit and spawn in the three major tributary drainages (Honey, Deep, and Twentymile Creeks). Large lake-dwelling populations of introduced fishes in the lakes likely reduce sucker recruitment by predation on young suckers (U.S. Fish and Wildlife Service 1998). The Recovery Plan for the Threatened and Rare Native Fishes of the Warner Basin and Alkali Subbasin (U.S. Fish and Wildlife Service 1998) sets recovery criteria for delisting the species. These criteria require that (1) a self-sustaining metapopulation is distributed throughout the Twentymile, Honey, and Deep Creek (below the falls) drainages, and in Pelican, Crump, and Hart Lakes, (2) passage is restored within and among the Twentymile, Honey, and Deep Creek (below the falls) drainages so that the individual populations of Warner suckers can function as a metapopulation, and (3) no threats exist that would likely threaten the survival of the species over a significant portion of its range. In 2008, we conducted investigations in Hart and Crump Lakes to quantify the abundance and distribution of Warner suckers, to search for evidence of recent recruitment, and to estimate sucker abundance relative to nonnative fish abundance. In addition we investigated growth and movement patterns. We used Passive Integrated Transponder (PIT) tagged suckers to determine growth rates and movements, tracked radio-tagged suckers to document seasonal spawning migrations, fished a screw trap in Twelvemile Creek to monitor downstream movements, and operated a trap at the Dyke diversion dam on Twentymile Creek to monitor upstream movements. Close

• 1592. [Article] 2017 Lostine Chinook Telemetry Study

  Abstract -- In this brief we present preliminary data from tracking the spawning migration of 75 (37 females and 38 males) adult spring Chinook in the Lostine River in 2017. Fish were radio-tagged at the ...

  Citation × Citation Citation Abstract Copy Title: 2017 Lostine Chinook Telemetry Study Abstract -- In this brief we present preliminary data from tracking the spawning migration of 75 (37 females and 38 males) adult spring Chinook in the Lostine River in 2017. Fish were radio-tagged at the Lostine River Weir from Jun 30 to Sep 1. Tagging was representative of run-timing. Radio-tagged fish were monitored continuously at four fixed antenna stations and weekly throughout the river using mobile antennas. Title: 2017 Lostine Chinook Telemetry Study Abstract -- In this brief we present preliminary data from tracking the spawning migration of 75 (37 females and 38 males) adult spring Chinook in the Lostine River in 2017. Fish were radio-tagged at the Lostine River Weir from Jun 30 to Sep 1. Tagging was representative of run-timing. Radio-tagged fish were monitored continuously at four fixed antenna stations and weekly throughout the river using mobile antennas. Close

• 1593. [Article] Passage behavior of radio-tagged yearling chinook salmon and steelhead at Bonneville Dam associated with the Surface Bypass Program, 2000

  Abstract -- In 1994, the U.S. Army Corps of Engineers (COE) initiated a program to develop and evaluate surface-oriented juvenile salmonid bypass systems at hydroelectric dams on the Columbia and Snake ...

  Citation × Citation Citation Abstract Copy Title: Passage behavior of radio-tagged yearling chinook salmon and steelhead at Bonneville Dam associated with the Surface Bypass Program, 2000 Abstract -- In 1994, the U.S. Army Corps of Engineers (COE) initiated a program to develop and evaluate surface-oriented juvenile salmonid bypass systems at hydroelectric dams on the Columbia and Snake rivers. The goal of the program was to develop juvenile bypass systems that would significantly improve the passage efficiency and survival of juvenile salmonids during their downstream migration. In 1998 a prototype surface collector (PSC) was installed at Bonneville Dam's first powerhouse. The PSC was designed not to bypass fish around the turbines but rather to examine fish behavior and hydraulics at the entrances and to determine the efficacy of surface bypass at BI before building a full production surface bypass system. In 1998 and 1999, our radio telemetry evaluation indicated that only 27-49% of the fish that came within 6 m of the entrances entered the PSC. We also determined that a 6 m entrance width was more efficient than a 1.5 m entrance width. In 2000, the PSC was extended to include turbines 1-6 and each of the six entrances was 6 m wide. To continue our evaluation of the PSC in 2000, we used radio telemetry to examine the movements and behavior of subyearling chinook salmon Oncorhynchus tshawytscha in the forebay of Bonneville Dam. The objectives of this research were to: 1) determine the behavior, distribution, and approach patterns of subyearling chinook salmon in the forebay areas of Bonneville Dam; 2) determine the time and route of dam passage of sub yearling chinook salmon; 3) determine movement patterns and behavior of subyearling chinook salmon in the vicinity of the PSC; and 4) assess the efficiency and effectiveness of the PSC. From 25 April to 1 June 2000, we radio-tagged and released 1,193 juvenile hatchery steelhead and 2,075 yearling chinook salmon. These fish were released from four locations upstream of Bonneville Dam: Rock Creek, John Day Dam, The Dalles Dam, and Hood River, Oregon. Median travel times from release to Bonneville Dam ranged from 14 h to 76 h, depending on species and the location of release. Of all the fish released, we detected 80% of steelhead and 82% of chinook salmon at Bonneville Dam. Of the fish released at Hood River, we detected 95% of steelhead and 94% of chinook salmon. Median residence time in the forebay areas of Bonneville Dam ranged from 8 min to 9 .7 h, depending on species and forebay area. Discharge rates and die! periods effected residence times of both species. Passage routes were determined for 91 % of steelhead and 92% of chinook salmon detected at Bonneville Dam. Nearly half ( 49%) of steelhead passed at powerhouse one (BI), and the largest proportion ( 44%) of chinook salmon passed through the spillway. Thirty-four percent of steelhead detected at Bonneville Dam passed through the spillway. Of the steelhead that passed at Bl, 44% passed into the sluiceway, 33% were guided into the downstream migration channel (DSM) via the standard-length submersible traveling screens (STS) or extended-length submersible bar screens (ESBS), and 23% were unguided and passed directly through the turbines. Of the chinook salmon that passed at Bl, 29% passed into the sluiceway, 36% were guided into the DSM, and 35% were unguided and passed directly through the turbines. Of the fish that passed at B2, 55% of steelhead and 39% of chinook salmon were guided into the DSM by the STS and 45% of steelhead and 60% of chinook salmon passed through the turbines unguided. No steelhead and 1 % of chinook salmon were detected passing through the sluice chute at B2, which was minimally operated during spring 2000. Passage rates were highest for both species during the day at the spillway and B 1. However, passage rates were highest for both species during the night at B2. Of the fish that entered the Bl forebay, 74% of steelhead and 63% of chinook sahnon were detected within 6 m of the PSC and were therefore considered to have discovered the PSC. Of the fish that discovered the PSC, 60% of steelhead and 72% of chinook salmon entered the PSC. However, of the fish that entered the PSC, only 29% (61 of 214) of steelhead and 41 % (100 of 246) of chinook salmon entered the PSC via the entrance they were first detected at without meandering to one or more entrances. Therefore, of the fish that entered the PSC, 71 % (153 of214) of steelhead and 59% (146 of 246) of chinook salmon meandered to one or more entrances before entering the PSC. In relation to units 1-6 at B 1, the PSC was quite efficient at collecting fish. Of the fish that passed at units 1-6 (guided and unguided) 83% of steelhead and 78% of chinook salmon entered the PSC. The PSC was also relatively effective compared to water passing into the turbines and the spillway. An effectiveness of 2.5 for steelhead and 2.4 for chinook salmon indicated that the proportion of fish that entered the PSC out of total passage at units 1-6 was over twice as high as the proportion of discharge that entered the PSC out of total discharge into and under the PSC at units 1-6. When compared to spillway effectiveness (1.0 for steelhead and 1.3 for chinook salmon), PSC effectiveness was about twice as high. Since fish that entered the PSC could pass through other routes, the PSC was not considered an actual passage route for purposes of calculating passage metrics such as FPE. However, if the PSC were an actual passage route, FPE would have increased from 78% to 85% for steelhead and from 73% to 78% for chinook salmon. Title: Passage behavior of radio-tagged yearling chinook salmon and steelhead at Bonneville Dam associated with the Surface Bypass Program, 2000 Abstract -- In 1994, the U.S. Army Corps of Engineers (COE) initiated a program to develop and evaluate surface-oriented juvenile salmonid bypass systems at hydroelectric dams on the Columbia and Snake rivers. The goal of the program was to develop juvenile bypass systems that would significantly improve the passage efficiency and survival of juvenile salmonids during their downstream migration. In 1998 a prototype surface collector (PSC) was installed at Bonneville Dam's first powerhouse. The PSC was designed not to bypass fish around the turbines but rather to examine fish behavior and hydraulics at the entrances and to determine the efficacy of surface bypass at BI before building a full production surface bypass system. In 1998 and 1999, our radio telemetry evaluation indicated that only 27-49% of the fish that came within 6 m of the entrances entered the PSC. We also determined that a 6 m entrance width was more efficient than a 1.5 m entrance width. In 2000, the PSC was extended to include turbines 1-6 and each of the six entrances was 6 m wide. To continue our evaluation of the PSC in 2000, we used radio telemetry to examine the movements and behavior of subyearling chinook salmon Oncorhynchus tshawytscha in the forebay of Bonneville Dam. The objectives of this research were to: 1) determine the behavior, distribution, and approach patterns of subyearling chinook salmon in the forebay areas of Bonneville Dam; 2) determine the time and route of dam passage of sub yearling chinook salmon; 3) determine movement patterns and behavior of subyearling chinook salmon in the vicinity of the PSC; and 4) assess the efficiency and effectiveness of the PSC. From 25 April to 1 June 2000, we radio-tagged and released 1,193 juvenile hatchery steelhead and 2,075 yearling chinook salmon. These fish were released from four locations upstream of Bonneville Dam: Rock Creek, John Day Dam, The Dalles Dam, and Hood River, Oregon. Median travel times from release to Bonneville Dam ranged from 14 h to 76 h, depending on species and the location of release. Of all the fish released, we detected 80% of steelhead and 82% of chinook salmon at Bonneville Dam. Of the fish released at Hood River, we detected 95% of steelhead and 94% of chinook salmon. Median residence time in the forebay areas of Bonneville Dam ranged from 8 min to 9 .7 h, depending on species and forebay area. Discharge rates and die! periods effected residence times of both species. Passage routes were determined for 91 % of steelhead and 92% of chinook salmon detected at Bonneville Dam. Nearly half ( 49%) of steelhead passed at powerhouse one (BI), and the largest proportion ( 44%) of chinook salmon passed through the spillway. Thirty-four percent of steelhead detected at Bonneville Dam passed through the spillway. Of the steelhead that passed at Bl, 44% passed into the sluiceway, 33% were guided into the downstream migration channel (DSM) via the standard-length submersible traveling screens (STS) or extended-length submersible bar screens (ESBS), and 23% were unguided and passed directly through the turbines. Of the chinook salmon that passed at Bl, 29% passed into the sluiceway, 36% were guided into the DSM, and 35% were unguided and passed directly through the turbines. Of the fish that passed at B2, 55% of steelhead and 39% of chinook salmon were guided into the DSM by the STS and 45% of steelhead and 60% of chinook salmon passed through the turbines unguided. No steelhead and 1 % of chinook salmon were detected passing through the sluice chute at B2, which was minimally operated during spring 2000. Passage rates were highest for both species during the day at the spillway and B 1. However, passage rates were highest for both species during the night at B2. Of the fish that entered the Bl forebay, 74% of steelhead and 63% of chinook sahnon were detected within 6 m of the PSC and were therefore considered to have discovered the PSC. Of the fish that discovered the PSC, 60% of steelhead and 72% of chinook salmon entered the PSC. However, of the fish that entered the PSC, only 29% (61 of 214) of steelhead and 41 % (100 of 246) of chinook salmon entered the PSC via the entrance they were first detected at without meandering to one or more entrances. Therefore, of the fish that entered the PSC, 71 % (153 of214) of steelhead and 59% (146 of 246) of chinook salmon meandered to one or more entrances before entering the PSC. In relation to units 1-6 at B 1, the PSC was quite efficient at collecting fish. Of the fish that passed at units 1-6 (guided and unguided) 83% of steelhead and 78% of chinook salmon entered the PSC. The PSC was also relatively effective compared to water passing into the turbines and the spillway. An effectiveness of 2.5 for steelhead and 2.4 for chinook salmon indicated that the proportion of fish that entered the PSC out of total passage at units 1-6 was over twice as high as the proportion of discharge that entered the PSC out of total discharge into and under the PSC at units 1-6. When compared to spillway effectiveness (1.0 for steelhead and 1.3 for chinook salmon), PSC effectiveness was about twice as high. Since fish that entered the PSC could pass through other routes, the PSC was not considered an actual passage route for purposes of calculating passage metrics such as FPE. However, if the PSC were an actual passage route, FPE would have increased from 78% to 85% for steelhead and from 73% to 78% for chinook salmon. Close

• 1594. [Article] Downstream rearing of juvenile Chinook salmon abundance, distribution and growth in the Upper Mainstem of the John Day River

  Abstract -- Juvenile spring Chinook (Oncorhynchus tshawytscha) emerge from the gravel in the late winter or early spring, and most follow a life history pattern known as Natal Reach Rearing (NRR) in which ...

  Citation × Citation Citation Abstract Copy Title: Downstream rearing of juvenile Chinook salmon abundance, distribution and growth in the Upper Mainstem of the John Day River Abstract -- Juvenile spring Chinook (Oncorhynchus tshawytscha) emerge from the gravel in the late winter or early spring, and most follow a life history pattern known as Natal Reach Rearing (NRR) in which juvenile fish remain in the stream reaches where they were spawned until their second spring of life when they start migrating towards the ocean (Healey 1991). However, in Columbia River tributaries, some juveniles have been observed following a Downstream Rearing (DSR) life history, in which they start moving downstream during their first spring towards other nursery habitats or perhaps ocean rearing (Copeland & Venditti 2009; Schroeder et al. 2016). Rearing in different habitats during their first year gives fish with these two life histories access to diverse food resources and, it is hypothesized that, this leads to different survival and growth advantages for these two groups. Differences in growth are of interest in efforts to conserve this threatened species because size is positively correlated to survival for salmon across multiple stages of their life cycle (Groot & Margolis 1991; Healey 1991; Quinn & Peterson 1996; Roni et al. 2012) Chinook salmon in the upper John Day River, Oregon, exhibit both NRR and DSR life history patterns. Fish following the DSR life history pattern are larger than NRR fish late in the spring, possibly due to factors such as higher fish density, lower stream productivity, and colder water temperatures in their natal reach than in the downstream reaches. However, this size advantage may be lost due to adverse summer conditions. Hot summer days combined with the withdrawal of water for agriculture lead to stream water temperatures well above lethal thresholds for salmon in many downstream reaches. DSR fish have been observed in tributaries of the mainstem John Day River, however their growth and survival during summer is unknown. Title: Downstream rearing of juvenile Chinook salmon abundance, distribution and growth in the Upper Mainstem of the John Day River Abstract -- Juvenile spring Chinook (Oncorhynchus tshawytscha) emerge from the gravel in the late winter or early spring, and most follow a life history pattern known as Natal Reach Rearing (NRR) in which juvenile fish remain in the stream reaches where they were spawned until their second spring of life when they start migrating towards the ocean (Healey 1991). However, in Columbia River tributaries, some juveniles have been observed following a Downstream Rearing (DSR) life history, in which they start moving downstream during their first spring towards other nursery habitats or perhaps ocean rearing (Copeland & Venditti 2009; Schroeder et al. 2016). Rearing in different habitats during their first year gives fish with these two life histories access to diverse food resources and, it is hypothesized that, this leads to different survival and growth advantages for these two groups. Differences in growth are of interest in efforts to conserve this threatened species because size is positively correlated to survival for salmon across multiple stages of their life cycle (Groot & Margolis 1991; Healey 1991; Quinn & Peterson 1996; Roni et al. 2012) Chinook salmon in the upper John Day River, Oregon, exhibit both NRR and DSR life history patterns. Fish following the DSR life history pattern are larger than NRR fish late in the spring, possibly due to factors such as higher fish density, lower stream productivity, and colder water temperatures in their natal reach than in the downstream reaches. However, this size advantage may be lost due to adverse summer conditions. Hot summer days combined with the withdrawal of water for agriculture lead to stream water temperatures well above lethal thresholds for salmon in many downstream reaches. DSR fish have been observed in tributaries of the mainstem John Day River, however their growth and survival during summer is unknown. Close

• 1595. [Article] Crooked River Fish Management Plan 1979

  Abstract -- The Crooked River is a major tributary to the Deschutes River and has the habitat to produce a good rainbow trout population, especially between Prineville Dam and Rice-Baldwin Dam. However, ...

  Citation × Citation Citation Abstract Copy Title: Crooked River Fish Management Plan 1979 Abstract -- The Crooked River is a major tributary to the Deschutes River and has the habitat to produce a good rainbow trout population, especially between Prineville Dam and Rice-Baldwin Dam. However, winter streamflow is minimal and high turbidity is common. The. river is not stocked but various ages and sizes of hatchery fish emigrate from Prineville Reservoir during periods of spill; and these fish constitute a sizable portion of the trout population in the river. The Crooked River has maintained a successful fishery on the combination of wild and hatchery (from Prinevi11e Reservoir) trout under general statewide regulations. In July 1979, the Oregon Fish and Wildlife Commission accepted the Department's recommendation to continue to manage this portion of Crooked River for wild and hatchery fish. Hatchery fish will not be stocked in this section of the river, but large numbers of hatchery trout migrate from Prineville Reservoir into the river below the dam. Title: Crooked River Fish Management Plan 1979 Abstract -- The Crooked River is a major tributary to the Deschutes River and has the habitat to produce a good rainbow trout population, especially between Prineville Dam and Rice-Baldwin Dam. However, winter streamflow is minimal and high turbidity is common. The. river is not stocked but various ages and sizes of hatchery fish emigrate from Prineville Reservoir during periods of spill; and these fish constitute a sizable portion of the trout population in the river. The Crooked River has maintained a successful fishery on the combination of wild and hatchery (from Prinevi11e Reservoir) trout under general statewide regulations. In July 1979, the Oregon Fish and Wildlife Commission accepted the Department's recommendation to continue to manage this portion of Crooked River for wild and hatchery fish. Hatchery fish will not be stocked in this section of the river, but large numbers of hatchery trout migrate from Prineville Reservoir into the river below the dam. Close

• 1596. [Article] Trout in Running Waters 1994 - Draft

  Abstract -- This chapter covers management of resident trout species in the Rogue, Applegate, and Illinois rivers and all associated tributary streams (running waters) of the Rogue River basin. Resident ...

  Citation × Citation Citation Abstract Copy Title: Trout in Running Waters 1994 - Draft Abstract -- This chapter covers management of resident trout species in the Rogue, Applegate, and Illinois rivers and all associated tributary streams (running waters) of the Rogue River basin. Resident rainbow and resident, fluvial, and anadromous cutthroat trout are native to the Rogue River basin. Angling for trout in the Rogue River basin did not become popular until the 1930s. At this time, cutthroat and downstream migrating steelhead were abundant and easily caught from streams in settled areas of the Rogue basin. Mining roads provided easy access to the headwaters of the Applegate and Illinois rivers, Jumpoff Joe creek, and Grave creek where trout fishing was most popular. The California-Oregon Power Company developed roads that provided access to trout fishing waters in the Prospect area in 1912 and the upper Rogue River and its tributaries became accessible in 1927 when the Crater Lake Highway was completed. The Civil Conservation corps developed foot paths and roads into remote parts of the basin in the 1930s. Trout fishing in high pressure areas in the Rogue basin is maintained by stocking. A list of species and numbers of hatchery fish stocked in running waters of the Rogue River basin is presented in Appendix Table A-4. Title: Trout in Running Waters 1994 - Draft Abstract -- This chapter covers management of resident trout species in the Rogue, Applegate, and Illinois rivers and all associated tributary streams (running waters) of the Rogue River basin. Resident rainbow and resident, fluvial, and anadromous cutthroat trout are native to the Rogue River basin. Angling for trout in the Rogue River basin did not become popular until the 1930s. At this time, cutthroat and downstream migrating steelhead were abundant and easily caught from streams in settled areas of the Rogue basin. Mining roads provided easy access to the headwaters of the Applegate and Illinois rivers, Jumpoff Joe creek, and Grave creek where trout fishing was most popular. The California-Oregon Power Company developed roads that provided access to trout fishing waters in the Prospect area in 1912 and the upper Rogue River and its tributaries became accessible in 1927 when the Crater Lake Highway was completed. The Civil Conservation corps developed foot paths and roads into remote parts of the basin in the 1930s. Trout fishing in high pressure areas in the Rogue basin is maintained by stocking. A list of species and numbers of hatchery fish stocked in running waters of the Rogue River basin is presented in Appendix Table A-4. Close

• 1597. [Article] Coho Life History in Tide Gated Lowland Coastal Streams, 2016-2018

  Abstract -- Coos Watershed Association’s (CoosWA) coho life history in tide gated lowland coastal streams, a life cycle monitoring (LCM) project, examines the ecology of tidal rearing for coho in the Coos ...

  Citation × Citation Citation Abstract Copy Title: Coho Life History in Tide Gated Lowland Coastal Streams, 2016-2018 Abstract -- Coos Watershed Association’s (CoosWA) coho life history in tide gated lowland coastal streams, a life cycle monitoring (LCM) project, examines the ecology of tidal rearing for coho in the Coos River Basin. This project has adapted to and advanced the recent paradigm shift in juvenile coho life histories, rearing and foraging strategies, growth, survival, migrations, and sub-basin level population productivity in the tidal zone. Temporal and spatial components of coho over-winter rearing strategies, in relation to habitat use and project effectiveness monitoring, is the monitoring focus in the paired study streams of Palouse and Willanch Creeks. Project results further reveal the fundamental mechanisms that promote juvenile coho growth and survival in the estuarine ecotone. In conjunction with prior and current data, results highlight the critical importance of these diverse habitats for recovering viable and resilient Oregon Coast coho populations. Title: Coho Life History in Tide Gated Lowland Coastal Streams, 2016-2018 Abstract -- Coos Watershed Association’s (CoosWA) coho life history in tide gated lowland coastal streams, a life cycle monitoring (LCM) project, examines the ecology of tidal rearing for coho in the Coos River Basin. This project has adapted to and advanced the recent paradigm shift in juvenile coho life histories, rearing and foraging strategies, growth, survival, migrations, and sub-basin level population productivity in the tidal zone. Temporal and spatial components of coho over-winter rearing strategies, in relation to habitat use and project effectiveness monitoring, is the monitoring focus in the paired study streams of Palouse and Willanch Creeks. Project results further reveal the fundamental mechanisms that promote juvenile coho growth and survival in the estuarine ecotone. In conjunction with prior and current data, results highlight the critical importance of these diverse habitats for recovering viable and resilient Oregon Coast coho populations. Close

• 1598. [Article] Abundance and life history characteristics of steelhead (Oncorhynchus mykiss) and Coho Salmon (Oncorhynchus kisutch) smolts in two direct ocean tributaries on the central Oregon coast, Information Report 2018-07

  Abstract -- In 1991, the Oregon Department of Fish and Wildlife (ODFW) began an intensive research study at Tenmile Creek on the central Oregon coast to evaluate the effects of a large wood addition on ...

  Citation × Citation Citation Abstract Copy Title: Abundance and life history characteristics of steelhead (Oncorhynchus mykiss) and Coho Salmon (Oncorhynchus kisutch) smolts in two direct ocean tributaries on the central Oregon coast, Information Report 2018-07 Abstract -- In 1991, the Oregon Department of Fish and Wildlife (ODFW) began an intensive research study at Tenmile Creek on the central Oregon coast to evaluate the effects of a large wood addition on juvenile salmonid populations. Nearby Cummins Creek served as a reference site. Annual monitoring of juvenile salmonid out-migrants began in 1992 at the two sites, continued through 2012 at Cummins Creek, and is ongoing at Tenmile Creek. These data offer an unusually long time-series of smolt abundance and life history characteristics for steelhead and Coho Salmon at monitoring sites located less than a kilometer from the point of ocean entry. Annual estimates of steelhead smolt abundance ranged from 740 to 3,236 smolts at Cummins Creek, and from 2,464 to 19,602 smolts at Tenmile Creek. For Coho Salmon, annual estimates ranged from 319 to 3,164 smolts at Cummins Creek, and from 1,637 to 11,553 smolts at Tenmile Creek. Steelhead smolt production at Tenmile Creek appeared to increase significantly relative to Cummins Creek following the large wood addition in 1996, but there was no evidence of a similar effect on Coho Salmon smolt production. Most steelhead smolts spent 2 years rearing in freshwater before out-migration, and we observed a higher proportion of age-1 smolts and lower proportion of age-3 smolts than several other studies in Oregon coastal streams. Coho Salmon smolt out-migrants were dominated by age-1 individuals at both sites, but there was evidence that some juvenile Coho Salmon out-migrated as age-0 smolts. Smolts of both species tended to be larger at Tenmile Creek than at Cummins Creek, and negative relationships between mean smolt size and smolt abundance suggest that rearing density may influence growth for juvenile salmonids in these streams. The median migration date of steelhead smolts was consistent over time and tracked closely between the two sites. Coho Salmon smolt out-migration timing was more variable and tended to be slightly later than for steelhead, particularly at Tenmile Creek. During peak migration, a high proportion of steelhead migrants classified as smolts based on length had body coloration consistent with smoltification. External signs of smoltification were not as prevalent among steelhead captured early in the season, particularly among smaller migrants. This long term out-migrant monitoring at the ocean entrance illustrates the variation that occurs in freshwater production and the patterns that occur in salmonid smolt life history but also shows that without spawner abundance data conclusions about freshwater production are limited. Title: Abundance and life history characteristics of steelhead (Oncorhynchus mykiss) and Coho Salmon (Oncorhynchus kisutch) smolts in two direct ocean tributaries on the central Oregon coast, Information Report 2018-07 Abstract -- In 1991, the Oregon Department of Fish and Wildlife (ODFW) began an intensive research study at Tenmile Creek on the central Oregon coast to evaluate the effects of a large wood addition on juvenile salmonid populations. Nearby Cummins Creek served as a reference site. Annual monitoring of juvenile salmonid out-migrants began in 1992 at the two sites, continued through 2012 at Cummins Creek, and is ongoing at Tenmile Creek. These data offer an unusually long time-series of smolt abundance and life history characteristics for steelhead and Coho Salmon at monitoring sites located less than a kilometer from the point of ocean entry. Annual estimates of steelhead smolt abundance ranged from 740 to 3,236 smolts at Cummins Creek, and from 2,464 to 19,602 smolts at Tenmile Creek. For Coho Salmon, annual estimates ranged from 319 to 3,164 smolts at Cummins Creek, and from 1,637 to 11,553 smolts at Tenmile Creek. Steelhead smolt production at Tenmile Creek appeared to increase significantly relative to Cummins Creek following the large wood addition in 1996, but there was no evidence of a similar effect on Coho Salmon smolt production. Most steelhead smolts spent 2 years rearing in freshwater before out-migration, and we observed a higher proportion of age-1 smolts and lower proportion of age-3 smolts than several other studies in Oregon coastal streams. Coho Salmon smolt out-migrants were dominated by age-1 individuals at both sites, but there was evidence that some juvenile Coho Salmon out-migrated as age-0 smolts. Smolts of both species tended to be larger at Tenmile Creek than at Cummins Creek, and negative relationships between mean smolt size and smolt abundance suggest that rearing density may influence growth for juvenile salmonids in these streams. The median migration date of steelhead smolts was consistent over time and tracked closely between the two sites. Coho Salmon smolt out-migration timing was more variable and tended to be slightly later than for steelhead, particularly at Tenmile Creek. During peak migration, a high proportion of steelhead migrants classified as smolts based on length had body coloration consistent with smoltification. External signs of smoltification were not as prevalent among steelhead captured early in the season, particularly among smaller migrants. This long term out-migrant monitoring at the ocean entrance illustrates the variation that occurs in freshwater production and the patterns that occur in salmonid smolt life history but also shows that without spawner abundance data conclusions about freshwater production are limited. Close

• 1599. [Article] Burnt River Basin Master Plan for Angler Access and Associated Recreational Uses 1966

  Abstract -- The Burnt River headwaters are found along the southwestern Baker County line. The North, South, and Middle Forks join at Unity Reservoir about five miles north of the town of Unity. Below ...

  Citation × Citation Citation Abstract Copy Title: Burnt River Basin Master Plan for Angler Access and Associated Recreational Uses 1966 Abstract -- The Burnt River headwaters are found along the southwestern Baker County line. The North, South, and Middle Forks join at Unity Reservoir about five miles north of the town of Unity. Below Unity Dam, the river makes its way through the Burnt River Valley. The 63.5 miles of the main river below Unity Dam is heavily infested with rough fish. To produce a good fishery, the river would need rehabilitation that would include: 1) Chemical treatment of the river and tributaries to remove the rough fish population. 2) Reintroduction of suitable fish species. 3) Construction of a barrier at downstream end to prevent upstream migration of rough fish from lower impoundments; e.g., Brownlee Reservoir. With the removal of rough fish, trout and warm-water game fish could be established and would produce good angling. At present, the trout fishery is confined to Unity Reservoir and the area directly below the dam. Trout angling on the forks of the system is limited and restricted to the early spring. Warm-water game fish are taken in the lower river in early spring. Title: Burnt River Basin Master Plan for Angler Access and Associated Recreational Uses 1966 Abstract -- The Burnt River headwaters are found along the southwestern Baker County line. The North, South, and Middle Forks join at Unity Reservoir about five miles north of the town of Unity. Below Unity Dam, the river makes its way through the Burnt River Valley. The 63.5 miles of the main river below Unity Dam is heavily infested with rough fish. To produce a good fishery, the river would need rehabilitation that would include: 1) Chemical treatment of the river and tributaries to remove the rough fish population. 2) Reintroduction of suitable fish species. 3) Construction of a barrier at downstream end to prevent upstream migration of rough fish from lower impoundments; e.g., Brownlee Reservoir. With the removal of rough fish, trout and warm-water game fish could be established and would produce good angling. At present, the trout fishery is confined to Unity Reservoir and the area directly below the dam. Trout angling on the forks of the system is limited and restricted to the early spring. Warm-water game fish are taken in the lower river in early spring. Close

• 1600. [Article] Grande Ronde River Basin Master Plan for Angler Access and Associated Recreational Uses 1966

  Abstract -- The Grande Ronde Basin is quite a large basin that drains most of the northeastern corner of our State. The system has five tributary rivers. Two are accessible by trail only, the Wenaha near ...

  Citation × Citation Citation Abstract Copy Title: Grande Ronde River Basin Master Plan for Angler Access and Associated Recreational Uses 1966 Abstract -- The Grande Ronde Basin is quite a large basin that drains most of the northeastern corner of our State. The system has five tributary rivers. Two are accessible by trail only, the Wenaha near the Washington state line and the Minam that flows northward between La Grande and Enterprise. Catherine Creek drains the upper eastern part of the Grande Ronde Valley; the Wallowa and Lostine Rivers flow out of the Wallowa Valley. The Grande Ronde system supports a good fishery for salmon and steelhead. These fish migrate up the Columbia and Snake Rivers and travel approximately 650 river miles before they reach the spawning areas in the upper reaches of the basin. The Lower Grande Ronde enjoys a fall steelhead fishery; the upper tributaries have spring salmon and in some instances spring steelhead. In the peak of the season angling pressure is heavy and success is good. This report details a plan that we hope can be followed to solve the access problems of the Grande Ronde Basin. Title: Grande Ronde River Basin Master Plan for Angler Access and Associated Recreational Uses 1966 Abstract -- The Grande Ronde Basin is quite a large basin that drains most of the northeastern corner of our State. The system has five tributary rivers. Two are accessible by trail only, the Wenaha near the Washington state line and the Minam that flows northward between La Grande and Enterprise. Catherine Creek drains the upper eastern part of the Grande Ronde Valley; the Wallowa and Lostine Rivers flow out of the Wallowa Valley. The Grande Ronde system supports a good fishery for salmon and steelhead. These fish migrate up the Columbia and Snake Rivers and travel approximately 650 river miles before they reach the spawning areas in the upper reaches of the basin. The Lower Grande Ronde enjoys a fall steelhead fishery; the upper tributaries have spring salmon and in some instances spring steelhead. In the peak of the season angling pressure is heavy and success is good. This report details a plan that we hope can be followed to solve the access problems of the Grande Ronde Basin. Close