Relocation and Recolonization of Coho Salmon in Two Tributaries to the Elwha River: Implications for Management and Monitoring
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Final Environmental Impact Statement
Final Environmental Impact Statement Elwha River Ecosystem Restoration Implementation Purpose and Need: The Elwha River ecosystem and native anadromous fisheries are severely degraded as a result of two hydroelectric dams (projects) and their reservoirs built in the early 1900s. Congress has mandated the full restoration of this ecosystem and its native anadromous fisheries through the Elwha River Ecosystem and Fisheries Restoration Act (Public Law 102-495). The Department of the Interior has found there is a need to return this river and the ecosystem to its natural, self-regulating state, and proposes to implement the Congressional mandate by removing both dams in a safe, environmentally sound and cost effective manner and implementing fisheries and ecosystem restoration planning. Only dam removal would fully restore the ecosystem or its native anadromous fisheries. Proposed Action: The U.S. Department of the Interior proposes to fully restore the Elwha River ecosystem and native anadromous fisheries through the removal of Elwha Dam and Glines Canyon Dam and implementing fish restoration and revegetation. Dam removal would occur over a 2-year period. Elwha Dam would be removed by blasting, and Glines Canyon Dam by a combination of blasting and diamond wire saw cutting. Lake Aldwell would be drained by a diversion channel, and Lake Mills by notching down Glines Canyon Dam. Stored sediment would be eroded naturally by the Elwha River. The proposed action is located in Clallam County, on the Olympic Peninsula, in Washington State. Lead/Cooperating agencies: The National Park Service is the lead agency. The U.S. Fish and Wildlife Service, U.S. -
Pacific Lamprey Restoration in the Elwha River Drainage Following Dam Removals Mary L
Pacific Lamprey Restoration in the Elwha River Drainage Following Dam Removals Mary L. Moser and Rebecca L. Paradis Spring 2017 American Currents 3 PACIFIC LAMPREY RESTORATION IN THE ELWHA RIVER DRAINAGE FOLLOWING DAM REMOVALS Mary L. Moser and Rebecca L. Paradis Northwest Fisheries Science Lower Elwha Klallam Tribe Natural Center, National Marine Resources, Port Angeles, WA Fisheries Service, Seattle, WA Dams and other man-made obstacles to fish passage fragment The Elwha River drainage historically supported a wide ar- riverine habitats and re-structure fish communities. Many of ray of anadromous species. Salmonids affected by these dams, these structures provide no means of fish passage or only par- including Bull Trout (Salvelinus confluentus), sea-run Cut- tial passage for a few species. This is particularly problematic throat (Oncorhynchus clarki), Steelhead (O. mykiss) and all five for diadromous and potamodromous species that must move species of Pacific salmon: Chinook O.( tshawytscha), Sockeye between rearing, feeding, and spawning habitats to complete (O. nerka), Chum (O. keta), Coho (O. kisutch), and Pink (O. their normal life cycle. In the United States and in Europe, gorbuscha) (Pess et al. 2008). Tribal elders described prolific many of these structures have become obsolete, and as a con- salmon runs prior to dam construction and legendary king sequence, dam removal has become a feasible fish restoration salmon of over 100 pounds each. One of the few remaining el- solution in many areas (Jackson and Moser 2012, Hogg et al. ders to have experienced the pre-dam fisheries recently passed 2013, Jolley et al. 2013, Lasne et al. -
Preface Preface
PREFACE PREFACE This Historic Structures Report was completed in accordance with examples of recreational development during the Forest Service the University of Oregon, Historic Preservation Masters program administration. The primary house refl ects the craftsman archi- and Terminal Project requirements. This report was also written tectural period and is the only remaining historic recreational resi- with the intention of assisting Olympic National Park in its stew- dence of this period and style owned by Olympic National Park. ardship of the presented historic buildings. The Wendel property was listed on the National Register of His- toric Places in 2005. An Historic Structures Report is a planning guide. The purpose of a Historic Structure Report to develop an assimilation of historic context and existing conditions of a building(s) to form the basis of recommendations on the care and conservation of the historic resource. The subject of the report is two structures located within Olympic National Park on the North shore of Lake Crescent, near the head of the Lyre River. The Wendel House and associated boathouse were built in 1936. The two structures are signifi cant Wendel House - Historic Structure Report Olympic National Park Page TABLE OF CONTENTS LIST OF FIGURES INTRODUCTION STATEMENT OF SIGNIFICANCE ADMINISTRATIVE DATA GEOGRAPHIC/NATURAL SETTING CHAPTER I: Historic Background Recreational Development The Olympics Before the Forest Reserve Olympic Forest Reserve 1893-1905 Recreational Development in the Olympics Before the National -
2.4 Elwha River and Tributaries Page 2.4-1
Chapter 2.4 Elwha River and Tributaries Page 2.4-1 2.4 ELWHA RIVER AND TRIBUTARIES 2.4.1 Overview The Elwha River is the largest watershed in the EMMT area and it constitutes the westernmost watershed within the planning area (Figure 2.4-1). The Elwha mainstem is approximately 45 miles long, has 100 miles of tributary streams, has a basin averaging approximately ten miles wide in an east-west direction, and drains 321 square miles of the Olympic Peninsula. Eighty-three percent of the drainage, including the upper 35 miles of the mainstem, lies within Olympic National Park, and is therefore protected from timber harvest, agriculture, and other land-use disturbances. The river flows in a northerly direction into the Strait of Juan de Fuca, entering the strait five miles west of Port Angeles. The Elwha is the fourth largest river, by drainage area, among all Olympic Peninsula streams, with a watershed area smaller only than those of the Quillayute, Queets, and Quinault rivers. Two major hydroelectric developments have altered the historic condition of the Elwha River. The Elwha Dam, built at RM 4.9 beginning in 1910, now impounds the 2.5-mile long Lake Aldwell reservoir, and the Glines Canyon Dam, built at RM 13.4, now impounds the 2.8-mile long Lake Mills reservoir. Originally built and operated to produce electricity for Port Angeles and beyond (supplying power as far away as Bremerton and Port Townsend prior to 1921), the dams have been fully allocated to supplying power to the pulp mill now operated by Nippon Paper Industries USA since the early 1920s. -
Abstract Joyner, Catelyn Nichole
ABSTRACT JOYNER, CATELYN NICHOLE. Lacustrine Megaturbidites and Displacement Waves: The Holocene Earthquake History of the Lake Creek-Boundary Creek Fault at Lake Crescent, Washington, USA. (Under the direction of Dr. Karl Wegmann and Dr. Elana Leithold). Lake Crescent is a deep, glacially carved lake located on the northern Olympic Peninsula within Olympic National Park. Its location in the forearc of the Cascadia subduction zone and proximity to seismically-active regional crustal faults allow for its high resolution sedimentary record to function as an extension of the local paleoseismic record. This study uses airborne lidar topography, multibeam bathymetry, seismic reflection profiles, and sediment cores to characterize four megaturbidites attributed to Holocene ruptures along the Lake Creek-Boundary Creek fault. The megaturbidites each consist of an erosively based normally graded basaltic sand layer overlain in turn by massive, homogenous silt with plant debris, a clay cap, and interstratified chloritic clay and basaltic sand laminae. The deposits can be traced across the deep basins of the 20 km2 lake and exceed 1.3 m in thickness in cores recovered from the deepest part of the lake. The youngest megaturbidite is estimated to have a minimum volume of ~4.8 x 106 m3. Petrologic analysis of megaturbidite basal sands indicates that they are sourced from the entire lake margin and likely were remobilized from shallow subaqueous environments. Newly acquired bathymetric data reveal that several large rockslides that surround Lake Crescent deposited debris into the lake. Previous research indicates that subaerial rockslides entering lakes can generate displacement (tsunami) waves and seiches that result in megaturbidite deposits. -
Open File Report 2003-6, Geologic Map of the Washington Portion Of
WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES OPEN FILE REPORT 2003-6 Division of Geology and Earth Resources Ron Teissere - State Geologist R. 3 W. 123°00¢ 48°30¢ Qgd Qgd Qgd Tertiary Sedimentary and Volcanic Rocks Pre-Tertiary Marine Metasedimentary Rocks JŠmco KJmmc KJmmc Qgt Qgd Qgdmes ROCKS OF THE CRESCENT TERRANE OF BABCOCK AND OTHERS (1994) KJmmc Constitution Formation (Cretataceous–Jurassic)—Poorly to moderately Qgdmes Qgt T. 35 N. KJmmc ROS sorted volcaniclastic sandstone, cherty sandstone, mudstone, and conglomer- Qf Qgd Twin River Group—Divided into: ate with less-abundant ribbon chert, green tuff, and basalt and dacite pillows; A RIO Qb MOm Pysht Formation (Miocene–Oligocene)—Massive, poorly indurated includes rare limestone. Clastic rock types are commonly massive and locally Qgd „…m p p marine mudstone, claystone, and sandy siltstone; also contains beds of graded; sandstone is commonly turbiditic; mudstone is commonly massive. THRUST very thick calcareous sandstone (1–20 ft thick). Unweathered mud- Conglomerate contains rounded to angular volcanic, chert, metaplutonic, and KJmmc Geologic Map of the Washington Portion of the Port Angeles 1:100,000 Quadrangle stone, claystone, and siltstone are medium gray to dark greenish gray, schistose clasts in a siltstone matrix; rhythmically bedded ribbon chert is JŠmco Qp Qgdmes pale yellowish brown where weathered. Mudstone locally contains thin commonly interbedded with clastic rocks throughout the unit but more abun- Qgdme T. 34 N. beds of calcareous claystone; argillaceous rocks commonly contain dant near the base. Green tuff occurs near base of section and is commonly fine grained and indurated; pillow lava is interlayered with clastic rocks; by Henry W. -
Final Technical Report May 31, 2017 USGS Award Number
College of Sciences Campus Box 8208 Department of Marine Earth & Atmospheric Sciences 1125 Jordan Hall 2800 Faucette Drive meas.ncsu.edu Raleigh, NC 27695-8208 Final Technical Report May 31, 2017 USGS Award Number: G15AP00091 Title of Award: Establishing a High-Resolution Post-Glacial Chronology of Surface Rupture on the Lake Creek—Boundary Creek Fault, Puget Sound Region, Washington State Authors & Affiliations: Karl W. Wegmanna, Elana L. Leitholdb, and DelWayne R. Bohnenstiehlc Department of Marine, Earth, and Atmospheric Sciences North Carolina State University 2800 Faucette Drive Raleigh, NC 27695-8208 a E-mail: [email protected]; Tel: 919-515-0380; Fax: 919-513-8812 b E-mail: [email protected]; Tel: 919-515-7282; Fax: 919-513-8812 c E-mail: [email protected]; Tel: 919-515-7449; Fax: 919-513-8812 Term Covered by Award: Start: July 1, 2015 End: February 28, 2017 Abstract: The Lake Creek–Boundary Creek fault and the Sadie Creek splay fault are similar to a number of steeply dipping crustal faults in the Puget Sound region exhibiting evidence for latest Pleistocene-Holocene surface rupture that accommodate north-south contraction and clockwise rotation of the Cascadia forearc in western Washington. The fault zone trends directly beneath Lake Crescent, which occupies a deep, glacially-scoured valley in Olympic National Park. There is direct physical evidence for surface ground rupture along at least 56 km of the fault zone both beneath Lake Crescent as well as to the west and east of the lake. Large Holocene landslide scarps surround the lake, and swath bathymetric data demonstrate that these failures deposited large masses of material into the lake itself. -
102317-Phewett
From: pearl hewett To: zSMP Cc: Ozias, Mark; ; Brian and Brooke; ; Tracy Horn; Sandy Rains; Delane Hewett; Vi; Van De Wege, Rep. Kevin; Office of Jesse Young; Mike Chapman; connie beauvais; Stephanie Noblin; Ivan Stocker; LIZ BOWEN; ; Sandy Collins; ; randy simmins; Wylie clark; Darol Johnson; Glen Morgan; Ross Krumpe; Louise Gliatto; RON SUSLICK; harry bell; Jim Boyer; Dick Pilling; Dan Clem; Rene"; Amanda Hewett; Art Ayres; Karl Spees; dianne L; Tyler, Ross; brian winter; Pam Roach; JOSH HOWARD; Winborn, Mary Ellen; Johnson, Randy; Peach, Bill; joni howard; Tristin Hewett; Lois Perry; Sue Forde; Rick Forschler -; Amy Cruver; levi howard; chuck cushman; Janet Fowler Subject: WDFW is considering public land for public access Date: Monday, October 23, 2017 12:54:53 PM Specifically, WDFW is considering public land for public access on the Elwha River Public Access to Public land is a really, really big deal on the 2017 Clallam County SMP Update THERE IS ONLY ONE SPOT OF/ FOR FREE PUBLIC ACCESS, ON LAKE SUTHERLAND A BOAT LAUNCH AND RESTROOM PROVIDED BY WDFW THE ACCESS SITE PROVIDES A CONCRETE PAD BOAT LAUNCH AND TOILETS. Lake Sutherland - Fish Washington | Washington Department of Fish ... wdfw.wa.gov/fishing/washington/473/ PLANTS OF TROUT INTO LAKE SUTHERLAND HAVE BEEN SUSPENDED WHILE DAM REMOVAL and ... THE WDFW ACCESS SITE PROVIDES A CONCRETE PAD BOAT LAUNCH AND TOILETS. Locate this lake This feature shows the general location of the selected body of water. Directions may not include routes to boat launches or other water access sites. Check below for access sites or read the description for specific access information. -
Paleoenvironmental Change on the Olympic Peninsula, Washington: Forests and Climate from the Last Glaciation to the Present
Paleoenvironmental Change on the Olympic Peninsula, Washington: Forests and Climate from the Last Glaciation to the Present Daniel G. Gavin1, David M. Fisher1, Erin M. Herring1, Ariana White1, and Linda B. Brubaker2 1. Department of Geography, University of Oregon, Eugene, Oregon. 2. School of Environment and Forest Sciences, University of Washington, Seattle, Washington. FINAL REPORT TO OLYMPIC NATIONAL PARK Contract J8W07100028 March 13, 2013 Table of Contents Acknowledgements ......................................................................................................... vii 1. Introduction ....................................................................................................................1 1.1 Aims of this report ............................................................................................................... 2 2. The modern landscape of the Olympic Peninsula .......................................................5 2.1 Geography of the Olympic Peninsula and Olympic National Park ................................ 5 2.2 Regional climate on the Olympic Peninsula ...................................................................... 5 2.3 Indicators of recent climate change on the Olympic Peninsula ....................................... 7 2.4 Vegetation zones of the Olympic Peninsula and climate controls on forest vegetation . 9 2.4.1 Sitka Spruce Zone ......................................................................................................... 10 2.4.2 Western Hemlock Zone ............................................................................................... -
An Assessment of Stream Habitat and Nutrients in the Elwha River Basin: Implications for Restoration
Prepared in cooperation with Lower Elwha Tribe and National Park Service An Assessment of Stream Habitat and Nutrients in the Elwha River Basin: Implications for Restoration 3y M.D. Munn, R.W. Black, A.L Haggland, M.A. Hummling, and R.L Huffman BRITISH COLUMBIA Elwha River Basin I 1 National Water-Quality Assessment Study Unit U.S. GEOLOGICAL SURVEY /Vater-Resources Investigations Report 98-4223 An Assessment of Stream Habitat and Nutrients in the Elwha River Basin: Implications for Restoration By M. D. Munn, R. W. Black, A. L. Haggland, M. A. Hummling, and R. L. Huffman U.S. GEOLOGICAL SURVEY Water-Resources Investigations Report 98-4223 Prepared in cooperation with the LOWER ELWHA TRIBE and NATIONAL PARK SERVICE Tacoma, Washington 1999 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Charles G. Groat, Director Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Geological Survey. For additional information write to: Copies of this report may be purchased from: District Chief U.S. Geological Survey U.S. Geological Survey Branch of Information Services 1201 Pacific Avenue, Suite 600 Box 25286 Tacoma, Washington 98402 Denver, Colorado 80225 Information regarding the National Water-Quality Assessment (NAWQA) Program is available on the Internet via the World Wide Web. You may connect to the NAWQA Home Page using the Universal Resource Locator (URL) at: <URL:http://wwwrvares.er.usgs.gov/nawqa/nawqa_home.html> FOREWORD Describe current water-quality conditions for a large part of the Nation's freshwater streams, rivers, and aquifers. -
Predicting Recolonization Patterns and Interactions Between
Samuel J. Brenkman1, National Park Service, Olympic National Park, 600 East Park Avenue, Port Angeles, Washington 98362 George R. Pess, NOAA Fisheries, Northwest Fisheries Science Center, 2725 Montlake Boulevard East, Seattle, Washington 98112 Christian E. Torgersen, U.S. Geological Survey, Forest and Rangeland Ecosystem Science Center, Cascadia Field Station, University of Washington, College of Forest Resources, Box 352100, Seattle, Washington 98195 Kristofer K. Kloehn, NOAA Fisheries, Northwest Fisheries Science Center, 2725 Montlake Boulevard East, Seattle, Washington 98112 Jeffrey J. Duda, U.S. Geological Survey, Western Fisheries Research Center, 6505 NE 65th Street, Seattle, Washington 98115 and Stephen C. Corbett, National Park Service, Olympic National Park, 600 East Park Avenue, Port Angeles, Washington 98362 Predicting Recolonization Patterns and Interactions Between Potamodromous and Anadromous Salmonids in Response to Dam Removal in the Elwha River, Washington State, USA Abstract The restoration of salmonids in the Elwha River following dam removal will cause interactions between anadromous and potamo- dromous forms as recolonization occurs in upstream and downstream directions. Anadromous salmonids are expected to recolonize historic habitats, and rainbow trout (Oncorhynchus mykiss) and bull trout (Salvelinus confluentus) isolated above the dams for 90 years are expected to reestablish anadromy. We summarized the distribution and abundance of potamodromous salmonids, determined locations of spawning areas, and mapped natural barriers to fish migration at the watershed scale based on data col- lected from 1993 to 2006. Rainbow trout were far more abundant than bull trout throughout the watershed and both species were distributed up to river km 71. Spawning locations for bull trout and rainbow trout occurred in areas where we anticipate returning anadromous fish to spawn. -
Dam Removal & the Elwha River
Ecosystem response to the removal of the Elwha River Dams Photo by John McMillan November 2018 K Denton & associates Location • 833 km2 • ~72km of mainstem habitat • 8 major tributaries • Sea level to 1,372m • Dry, warm summers and cool, wet winters • Marine sedimentary, Crescent basalt, and Unconsolidated glacial till • Western hemlock, Douglas Fir, Western Red Cedar, Red alder, cottonwood, and big leaf maple Location Elwha River Fishes John McMillan John McMillan Coho salmon Pink salmon Chinook salmon John McMillan Jonny Armstrong Steelhead Chum salmon Sockeye salmon Jonny Armstrong John McMillan Eulachon Bull trout Pacific lamprey John McMillan Purpose Elwha River Ecosystem and Fisheries Restoration Act “…for the removal of the dams and full restoration of the Elwha River ecosystem and native anadromous fisheries.” 102nd Congress of the U.S.A. January 3, 1992 Photo by John McMillan Dam removal will result in fish passage to the Elwha River Elwha Dam Glines Canyon Dam > 90% of habitat inaccessible Dam removal will result in fish passage to the Elwha River Elwha Dam Glines Canyon Dam Restored sediment dynamics will result in the creation & maintenance of existing and “lost” habitats Elwha River mouth 2006 Elwha River mouth 2015 0.5km 1km Restored connectivity for fish and sediment dynamics will lead to restored riverine foodwebs, terrestrial linkages, and revegetation Bellmore et al. in press Study design Location Dams & former reservoirs Nearshore River ecosystem Processes Sediment dynamics Fish recolonization Riverine foodwebs Terrestrial linkages Revegetation Study design Experimental design Spatial design Temporal design Adult fish Multiple Stratified systematic survey Daily, weekly, & before/after/ (SSS) seasonal Control/impact Opportunistic (O) (MBACI) Juvenile fish BACI SSS/O Monthly, seasonal, & annual Foodwebs MBACI SSS/O Seasonal Habitats BA SSS/Census Annual Sediment BA SSS Daily, seasonal Riparian BA SSS/O Seasonal, annual .