Idaho Power Company's Fall Chinook Salmon Hatchery
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Clean Water Act Section 401 Water Quality Certification Hells Canyon Complex (FERC Project Number 1971)
Evaluation and Findings Report: Clean Water Act Section 401 Water Quality Certification Hells Canyon Complex (FERC Project Number 1971) May 2019 Northwest Region 700 NE Multnomah St. Suite 600 Portland, OR 97232 Phone: 503-229-5696 800-452-4011 Fax: 503-229-5850 www.oregon.gov/DEQ DEQ is a leader in restoring, maintaining and enhancing the quality of Oregon’s air, land and water. Oregon Department of Environmental Quality 401 Water Quality Certification Hells Canyon Complex (FERC Project Number 1971) This report prepared by: Oregon Department of Environmental Quality 700 NE Multnomah St Suite 600 Portland, OR 97232 1-800-452-4011 www.oregon.gov/deq Contact: Marilyn Fonseca 503-229-6804 Documents can be provided upon request in an alternate format for individuals with disabilities or in a language other than English for people with limited English skills. To request a document in another format or language, call DEQ in Portland at 503-229-5696, or toll-free in Oregon at 1-800-452-4011, ext. 5696; or email [email protected]. State of Oregon Department of Environmental Quality ii 401 Water Quality Certification Hells Canyon Complex (FERC Project Number 1971) Table of Contents 1 Introduction ......................................................................................................................................... 1 2 Requirements for Certification ............................................................................................................ 1 2.1 Applicable Federal and State Law .............................................................................................. -
Dams and Hydroelectricity in the Columbia
COLUMBIA RIVER BASIN: DAMS AND HYDROELECTRICITY The power of falling water can be converted to hydroelectricity A Powerful River Major mountain ranges and large volumes of river flows into the Pacific—make the Columbia precipitation are the foundation for the Columbia one of the most powerful rivers in North America. River Basin. The large volumes of annual runoff, The entire Columbia River on both sides of combined with changes in elevation—from the the border is one of the most hydroelectrically river’s headwaters at Canal Flats in BC’s Rocky developed river systems in the world, with more Mountain Trench, to Astoria, Oregon, where the than 470 dams on the main stem and tributaries. Two Countries: One River Changing Water Levels Most dams on the Columbia River system were built between Deciding how to release and store water in the Canadian the 1940s and 1980s. They are part of a coordinated water Columbia River system is a complex process. Decision-makers management system guided by the 1964 Columbia River Treaty must balance obligations under the CRT (flood control and (CRT) between Canada and the United States. The CRT: power generation) with regional and provincial concerns such as ecosystems, recreation and cultural values. 1. coordinates flood control 2. optimizes hydroelectricity generation on both sides of the STORING AND RELEASING WATER border. The ability to store water in reservoirs behind dams means water can be released when it’s needed for fisheries, flood control, hydroelectricity, irrigation, recreation and transportation. Managing the River Releasing water to meet these needs influences water levels throughout the year and explains why water levels The Columbia River system includes creeks, glaciers, lakes, change frequently. -
The Hells Canyon Dam Controversy
N 1956, AT THE TENDER AGE OF THIRTY-TWO, Frank Church made a bold bid for the United States Senate. After squeak- I ing out a victory in the hotly contested Idaho Democratic pri- mary, Church faced down incumbent Senator Herman Welker, re- ceiving nearly percent of the vote. One issue that loomed over the campaign was an emerging dis- pute over building dams in the Snake River’s Hells Canyon. While Church and other Democrats supported the construction of a high federal dam in the Idaho gorge, their Republican opponents favored developing the resource through private utility companies. Idaho EVOLUTION voters split on the issue, and so, seeking to avoid a divisive debate, Church downplayed his position during the general election “be- of an cause it was not a winning issue, politically.”1 Senator Frank Church Although Church won the election, he could not escape the is- sue. Indeed, his victory and subsequent assignment to the Senate Committee on Interior and Insular Affairs put him at the center of a growing controversy about damming Hells Canyon. Over the next eighteen years, Church wrestled with balancing Idaho’s demand for economic growth and his own pro-development beliefs with an emerging environmental movement’s demand for preservation of nature—in Idaho and across the nation. As he grappled with these competing interests, Church under- went a significant transformation. While Church often supported development early in his Senate career, he, like few others of his time, began to see the value of wild places and to believe that rivers offered more than power production opportunities and irrigation water. -
Snake River Fall Chinook a Primer: 1900-1975
Snake River Fall Chinook A Primer: 1900-1975 Mark Schuck – Washington Department of Fish and Wildlife. Acknowledgements and note to the reader. The majority of the structure of the presentation was developed by Dr. Billy Connor (USFWS) and through extensive history research by Jim Chandler (Idaho Power Company). Additional insights and historical perspective were provided by several persons from numerous agencies involved with fall Chinook management {Stuart Rosenberger, IPC - GIS Division, Jay Hesse (NPT), Pete Hassemer (IDFG), and several other biologist and researchers that indirectly provided data for slides}. It was my privilege to assemble that information into this presentation. While some of the content from slides in the original presentation provided to the ISRP and attendees on August 6, 2013 will be included in this narrative and slide references are provided in the text that follows, I suggest the best approach to reviewing the history is to read this in concert with the slide presentation, available on the LSRCP website at: http://www.fws.gov/lsnakecomplan/ The purposes of this overview are: • Provide a history of the near demise of Snake Fall Chinook • Review the actions that resulted in the need for, and authorization of, the LSRCP in 1975 • Put everyone on the same plane so that they better understand fall Chinook history • Provide context to better evaluate the success or failure of the LSRCP fall Chinook program, because: We can’t know where we are going if we don’t know where we’ve been. Introduction Chinook are a cultural icon of the Pacific Northwest. King, Tyee or Chinook, the terms convey the aura of big hard fighting fish of the most splendid flavor. -
Snake River Flow Augmentation Impact Analysis Appendix
SNAKE RIVER FLOW AUGMENTATION IMPACT ANALYSIS APPENDIX Prepared for the U.S. Army Corps of Engineers Walla Walla District’s Lower Snake River Juvenile Salmon Migration Feasibility Study and Environmental Impact Statement United States Department of the Interior Bureau of Reclamation Pacific Northwest Region Boise, Idaho February 1999 Acronyms and Abbreviations (Includes some common acronyms and abbreviations that may not appear in this document) 1427i A scenario in this analysis that provides up to 1,427,000 acre-feet of flow augmentation with large drawdown of Reclamation reservoirs. 1427r A scenario in this analysis that provides up to 1,427,000 acre-feet of flow augmentation with reservoir elevations maintained near current levels. BA Biological assessment BEA Bureau of Economic Analysis (U.S. Department of Commerce) BETTER Box Exchange Transport Temperature Ecology Reservoir (a water quality model) BIA Bureau of Indian Affairs BID Burley Irrigation District BIOP Biological opinion BLM Bureau of Land Management B.P. Before present BPA Bonneville Power Administration CES Conservation Extension Service cfs Cubic feet per second Corps U.S. Army Corps of Engineers CRFMP Columbia River Fish Mitigation Program CRP Conservation Reserve Program CVPIA Central Valley Project Improvement Act CWA Clean Water Act DO Dissolved Oxygen Acronyms and Abbreviations (Includes some common acronyms and abbreviations that may not appear in this document) DREW Drawdown Regional Economic Workgroup DDT Dichlorodiphenyltrichloroethane EIS Environmental Impact Statement EP Effective Precipitation EPA Environmental Protection Agency ESA Endangered Species Act ETAW Evapotranspiration of Applied Water FCRPS Federal Columbia River Power System FERC Federal Energy Regulatory Commission FIRE Finance, investment, and real estate HCNRA Hells Canyon National Recreation Area HUC Hydrologic unit code I.C. -
PASSAGE ·OF ADULT FALL-RUN CHINOOK SALMON (Oncorhynchus T�Hawytscha) THROUGH a LARGE IMPOUNDMENT
\� PASSAGE ·OF ADULT FALL-RUN CHINOOK SALMON (Oncorhynchus t�hawytscha) THROUGH A LARGE IMPOUNDMENT by Parker s. Trefethen and Doyle F. Sutherland July 1964 FISH-PASSAGE RESEARCH PROGRAM· - Bureau of Commercial Fisheries Seattle, Washington INTRODUCTION One of the basic considerations in planning for--fish passage at high dams is the effect of a large, deep impoundment on the upstream migration of adult salmon. If anadromous fish can pass through a large impoundment and successfully spawn, they may be passed directly over the dam into the forebay to continue their natural migration. If passage in the reservoir is impaired, it may be necessary to transport the fish around the reservoir- an operation that may be complicated by the need for separating subpopulations in the event that several tributary streams are involved. The effect of a large impoundment on the passage of adult salmon was examined in Bro�nlee Reservoir on the Snake River (fig. 1). This 57�-mile-long impoundment, created in 1958, presented a potential barrier to chinook salmon (O. tshawytscha) and steelhead trout (Salmo gairdneri} on their upstream migration to spawning areas above the reservoir. Except during extreme drawdown and high river discharges, virtually no water currents ex.1st in the impoundment, and high temperatures & low oxygen concentrations are prevalent--especially during summer and fall - months. Since the filling of Brownlee Reservoir, the number of adult salmon returning to the area has declined. There may be many factors responsible for this decline, but at the outset of these studies it was recognized that adult fish might experience difficulty in migrating through the large impoundment to spawning areas. -
Spawning Areas and Abundance of Chinook Salmon {Oncorhynchus Tshawytscha} in the Columbia River Basin--Past and Present By
UNITED STATES DEPARTMENT OF THE INTERIOR u.S. FISH AND WILDLIFE SERVICE BUREAU OF COMMERCIAL FISHERIES Spawning Areas and Abundance of Chinook Salmon {Oncorhynchus tshawytscha} in The Columbia River Basin--Past and Present By LEONARD A. FULTON United States Fish and Wildlife Service Special Scientific Report- - Fisheries No. 571 Washington, D.C. October 1968 CONTENTS Page Introduction........................ Spring- and summer-run chinook salmon. .. 3 Spawning areas . .. 3 Abundance of spring- and summer- run chinook salmon. 4 Fall-run chinook salmon. 16 Spawning areas . 16 Abundance of fall- run chinook salmon 20 Summary and conclusions 22 Acknowledgments. 23 Literature cited .. 24 Maps .............. .See Map Appendix iii Spawning Areas and Abundance of Chinook Salmon (Oncorhynchus tshawytscha) in The Columbia River Basin--Past and Present By LEONARD A. FULTON, Fishery Biologist Bureau of Commercial Fisheries 'Biological Laboratory Seattle, Washington 98102 ABSTRACT Chinook salmon, the most abundant species of salmon in the Columbia Basin, formerly spawned in nearly a11 tributaries ofthe Columbia River and in many areas of the main river. Over the past 60 years, the construction of dams has inundated, impeded, or blocke.d acces!, to spawning areas. Despite these heavy losses, large areas of spawning grounds in the middle and lower portions of the drainage are sti11 available to chinook salmon. Stream im provements by State and Federal fishery agencies have rehabilitated some areas and have brought others into production for the first time. Important spawning areas are listed and charted in this report according to their past use (before 1965) and present use (1966). Estimates of recent spawning populations in major tributaries and in segments of the main stem are also given. -
Endangered Species Act 1972 1855 Treaties U.S. and Nez Perce
Harvest Pacific Salmon Treaty (Pacific Salmon Hydro/Habitat Commission - PSC) Federal Columbia River Power System Magnuson Act (Pacific Fishery Biological Opinion Management Council – PFMC) • Dworshak Dam Endangered SpeciesSnake/Columbia Act 1972 summer spill U.S. vs. Oregon Management Agreement • Federal Energy Regulatory Commission • Idaho Power Complex Snake River Synergy is the interaction of elements that when combined produce a total effect that Fall Chinook is greater than the sum of the individual Salmon elements Hatchery Idaho Power Company/Hells Canyon Settlement Agreement Lower1855 Snake River Treaties Compensation U.S. Plan – Publicand Law Nez 94-587, Perce, 99-662, 103-316 NorthwestUmatilla,Yakama Power Act & Warm Springs U.S. vs. Oregon Management Agreement Columbia Basin Treaty Tribes Accords Snake River Falls SEA K 14% PFMC 34% CA NA DA 52% Pacific Salmon Treaty (Pacific Salmon Commission - PSC) Magnuson Act (Pacific Fishery Management Council – PFMC) U.S. vs. Oregon Management Agreement Columbia River Treaty Tribe Harvest Hydro/Habitat Federal Energy Regulatory Commission • Idaho Power Complex Federal Columbia River Power System Biological Opinion & Litigation • Snake/Columbia summer spill Snake River • Juvenile Transportation • Predation Fall Chinook • Estuary Salmon Bonneville Dam 1938 BrownleeIce Harbor Dam 1961 1958 LowerTheOxbow DallesMonumental Dam Dam 1961 1957 Dam 1969 John Day Dam 1971 HellsLittle Canyon Goose DamDam 19671970 Lower Granite Dam 1975 McNary Dam 1954 Warner W. Gardner, Assistant Secretary of the -
Snake River Fall Chinook Brood Origin
Lyons Ferry Hatchery and Production of Snake River Fall Chinook: A Qualified Success Story. Mark Schuck Washington Department of Fish and Wildlife Lower Snake River Fish and Wildlife Compensation Plan - 1976 • Fall Chinook – 18,300 adults/year • Tucannon Spring Chinook – 1,132 adults/year to the river • Summer Steelhead – 4,656 adults/year to project rivers • In-place and in-kind (genetic integrity) • Resident fish – fishing opportunity – 67,500 angler days LFH Fall Chinook Production Goals (18,300 adults) • 9.16 million subyearling smolts (101,880 lbs) – about 90 fpp (80 mm) – expected smolt-to-adult return (SAR) of 0.2% • Idaho Power Co. mitigation for Hells Canyon Complex – for 1.3 million eyed eggs – due after LFH reached 80% of capacity • Program to be built from Endemic Snake Chinook Snake River Fall Chinook Salmon Population and ESU Structure er iv R Missoula e wa ## s lear ter R WASHINGTON ou C al k C P r Snake River o Pullman o l # #Moscow F u m $LOWER GRANITE DAM N • One remaining b LOWER MONUMENTAL DAM Fall Chinook ia $ $ LITTLE GOOSE DAM er R R at rw i Tu ea r v c l e R a C iv e R n # L k a r e n k Lewiston o e s o h a lo e c Richland et River n r # n uch S C o Pasco S n L # $ o R T a population # ICE HARBOR DAM iv Fall Chinook ESU Kennewick er k e Walla Walla Walla Walla S R F R # de on C S MONTANA MCNARY DAM R l e e l $ e w n d a current fall ra r a G w y R R a ter R –Lyons Ferry Hatchery chinook spawning iv U e i r v m e at r il la# River Wa Pendleton llow historic fall a Sa R lm M i o genetics very similar to chinook spawning -
PO Box 579 Coeur D'alene, Idaho 83816-0579 \ 800.451.6034 \ Fax
PO Box 579 Coeur d’Alene, Idaho 83816-0579 ⏐ 800.451.6034 ⏐ fax: 208.667.6506 ⏐ [email protected] Sharing Nature~Enriching Lives. Since 1979. SNAKE RIVER HIKE JOURNEY THROUGH HELLS CANYON In 1989, ROW Adventures pioneered the concept of raft-supported Idaho hiking and walking tours. Our walking trips and hiking vacations allow you to comforta- bly follow an isolated river's path on foot while a cargo raft carries your camp gear. You can enjoy the scenery and photograph wildlife, carrying only water and a small daypack. Each hiking trip is accompanied by one of our expert interpre- tive guides for area education and safety. Each day you hike between five and ten miles on wilderness trails that roughly parallel the river's course. Elevation on these trails is generally moderate. Hiking clubs, groups of friends and active boomers have all joined our Idaho hiking trips and experienced these superlative walking tours. TABLE OF CONTENTS 1 INTRODUCTION 2 AT A GLANCE 3 ABOUT THE REGION 4 TRIP EXTENSIONS 6 GETTING THERE"! 7 ITINERARY 8 SNAKE RIVE LORE 9 SUSTAINABLE TRAVEL! 10 TRIP DETAILS! 11 TERMS AND CONDITIONS! 13 WHY ROW AT A GLANCE DURATION 5 days INTENSITY Intermediate SEASON May, June and September MINIMUM AGE 12 BEGINS IN Cambridge, Idaho ENDS IN Lewiston, Idaho AIRPORT Begin: Boise, ID; End: Lewiston, ID TRIP DATES! Call for specific departure dates. TRIP COSTS! Starting at $1495 TRIP INCLUDES Services of our talented adventure consultants and pro- fessional guides, all meals/beverages as indicated in itinerary, transportation from Boise to Cambridge DOES NOT INCLUDE! Airfare/transportation beginning and ending points, van shuttle if you arrive in Boise after 4pm, gratuities, travel protection plan, pre-& post-trip hotel, items of a personal nature 2 IDAHO’S SNAKE RIVER Hiking the Snake River lets you experience the beauty of the deepest canyon in North America. -
“Grand Canyon of the Snake River,” the Hells Canyon Corridor Is Known for Its Magnificent but Extremely Rugged Landscape
95 THE 12 HELLS 95 CANYON 95 CORRIDOR WHAT’S IT LIKE? Once called the “Grand Canyon of the Snake River,” the Hells Canyon corridor is known for its magnificent but extremely rugged landscape. Seven Devils Mountains There are few points of entry into Hells Canyon, so traveling in this corridor takes time and effort. Company road to Hells Canyon Creek. This Once there, however, visitors are rewarded with paved two-lane road twists through ranch land to indescribably beautiful scenery and exciting Oxbow Dam, where it follows the Snake River to whitewater on the wild and scenic Snake River. Hells Canyon Dam. At Hells Canyon Dam the There are unlimited opportunities for camping, road crosses to the Oregon side of the canyon and hiking or just admiring the ever-changing views. ends 1.5 miles at the Hells Canyon Creek Recre- ation Site. WHAT’S THE ROAD LIKE? Access to the Hells Canyon Wilderness in the Highway District Road 493, which intersects Seven Devils Mountains is from Forest Road 517 Highway 95 near White Bird and winds 20 miles near Riggins. The last seven miles was improved to Pittsburg Landing, is one of two Idaho access so that passenger cars are able to access the area. points to the Snake River in Hells Canyon. The The steep and winding single-lane gravel road is road is a single-lane gravel road with steep grades not recommended for RVs or vehicles towing and tight switchbacks. camping trailers. The other Idaho access point to the Snake River Since weather and road conditions change is County Road 71, which intersects Highway 95 quickly, it is strongly recommended that travelers at Cambridge and traverses 65 miles to call the Hells Canyon National Recreation Area Copperfield where it meets the Idaho Power office in Riggins before beginning any adventure in Hells Canyon. -
Snake River Fall Chinook a Primer:1900-1975
Snake River Fall Chinook A Primer:1900-1975 Mark Schuck Washington Department of Fish and Wildlife Acknowledgements • Staff from many agencies contributed to this presentation – without which it would not exist! • A few notable contributors: – Billy Connor, Jim Chandler, Stuart Rosenberger, IPC - GIS Division, Jay Hesse, Pete Hassemer • Our funding Entities – Purpose of this Presentation • History of the near demise of Snake Fall Chinook • Review the actions that resulted in the need for and authorization of the LSRCP in 1975 • Put everyone on the same plane so that they better understand fall Chinook history • Can’t know where we are going if we don’t know where we’ve been “Chinook” • Cultural Icon – King, Tyee • Legendary size and Columbia R. abundance • Staple food of native peoples • Adaptive – Spring, summer, fall runs • Upriver Bright falls for Snake – big mainstem spawners. • Snake – historically large producer of Chinook Maladies for Decline • Anthropogenic – Over harvest – Habitat loss • Irrigated Agriculture (water removal + sediments) • Logging • Gold Dredging • Dam construction – Hatchery efforts w/ questionable old methods • Natural – Drought – Ocean Productivity Possible historic distribution of habitat utilized by fall Chinook salmon Typical Pre-development Snake Habitat Thousand Springs region of Snake R. (1902). Eastern Snake Aquifer had significant effect on thermal regime of the Snake River in historical fall Chinook core spawning area. Collectively springs contributed 4,000 to 5,000 cfs of 58 Degree F. inflow. (USGS Survey library) Typical Pre-development Snake Habitat Photo of Millett Island (1902), just below Upper Salmon Falls. Historic monitoring site for fall Chinook spawning. Described in Everman, c. 1894. (USGS Survey library) Typical Pre-development Snake Habitat Photo of Lower Salmon Falls (1902).