Seasonal Distribution and Habitat Associations of Salmonids With
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Suspended-Sediment Concentration in the Sauk River, Washington, Water Years 2012-13
Prepared in cooperation with the Sauk-Suiattle Indian Tribe Suspended-Sediment Concentration in the Sauk River, Washington, Water Years 2012-13 By Christopher A. Curran1, Scott Morris2, and James R. Foreman1 1 U.S. Geological Survey, Washington Water Science Center, Tacoma, Washington 2 Department of Natural Resources, Sauk-Suiattle Indian Tribe, Darrington, Washington Photograph of glacier-derived suspended sediment entering the Sauk River immediately downstream of the Suiattle River mouth (August 5, 2014, Chris Curran). iii Introduction The Sauk River is one of the few remaining large, glacier-fed rivers in western Washington that is unconstrained by dams and drains a relatively undisturbed landscape along the western slope of the Cascade Range. The river and its tributaries are important spawning ground and habitat for endangered Chinook salmon (Beamer and others, 2005) and also the primary conveyors of meltwater and sediment from Glacier Peak, an active volcano (fig. 1). As such, the Sauk River is a significant tributary source of both fish and fluvial sediment to the Skagit River, the largest river in western Washington that enters Puget Sound. Because of its location and function, the Sauk River basin presents a unique opportunity in the Puget Sound region for studying the sediment load derived from receding glaciers and the potential impacts to fish spawning and rearing habitat, and downstream river-restoration and flood- control projects. The lower reach of the Sauk River has some of the highest rates of incubation mortality for Chinook salmon in the Skagit River basin, a fact attributed to unusually high deposition of fine-grained sediments (Beamer, 2000b). -
Skagit River Emergency Bank Stabilization And
United States Department of the Interior FISH AND WILDLIFE SERVICE Washington Fish and Wildlife Office 510 Desmond Dr. SE, Suite 102 Lacey, Washington 98503 In Reply Refer To: AUG 1 6 2011 13410-2011-F-0141 13410-2010-F-0175 Daniel M. Mathis, Division Adnlinistrator Federal Highway Administration ATIN: Jeff Horton Evergreen Plaza Building 711 Capitol Way South, Suite 501 Olympia, Washington 98501-1284 Michelle Walker, Chief, Regulatory Branch Seattle District, Corps of Engineers ATIN: Rebecca McAndrew P.O. Box 3755 Seattle, Washington 98124-3755 Dear Mr. Mathis and Ms. Walker: This document transmits the U.S. Fish and Wildlife Service's Biological Opinion (Opinion) based on our review of the proposed State Route 20, Skagit River Emergency Bank Stabilization and Chronic Environmental Deficiency Project in Skagit County, Washington, and its effects on the bull trout (Salve linus conjluentus), marbled murrelet (Brachyramphus marmoratus), northern spotted owl (Strix occidentalis caurina), and designated bull trout critical habitat, in accordance with section 7 of the Endangered Species Act of 1973, as amended (16 U.S.C. 1531 et seq.) (Act). Your requests for initiation of formal consultation were received on February 3, 2011, and January 19,2010. The Federal Highway Administration (FHWA) and U.S. Army Corps of Engineers - Seattle District (Corps) provided information in support of "may affect, likely to adversely affect" determinations for the bull trout and designated bull trout critical habitat. On April 13 and 14, 2011, the FHWA and Corps gave their consent for addressing potential adverse effects to the bull trout and bull trout critical habitat with a single Opinion. -
Schedule of Proposed Action (SOPA)
Schedule of Proposed Action (SOPA) 01/01/2015 to 03/31/2015 Mt Baker-Snoqualmie National Forest This report contains the best available information at the time of publication. Questions may be directed to the Project Contact. Expected Project Name Project Purpose Planning Status Decision Implementation Project Contact R6 - Pacific Northwest Region, Regionwide (excluding Projects occurring in more than one Region) Aquatic Invasive Species order - Wildlife, Fish, Rare plants In Progress: Expected:04/2015 05/2015 James Capurso to prevent the spread or Scoping Start 05/05/2014 208-557-5780 introduction of aquatic invasive [email protected] species Description: The purpose of this order is to prevent the spread or introduction of aquatic invasive plant or animal species. CE Public involvement is targeted for the Umatilla, Willamette, Mt. Baker-Snoqualmie, Gifford Pinchot, and Colville NFs. Web Link: http://www.fs.fed.us/nepa/nepa_project_exp.php?project=44360 Location: UNIT - R6 - Pacific Northwest Region All Units. STATE - Oregon, Washington. COUNTY - Asotin, Clark, Columbia, Cowlitz, Ferry, Garfield, King, Klickitat, Lewis, Pend Oreille, Pierce, Skagit, Skamania, Snohomish, Stevens, Walla Walla, Whatcom, Baker, Clackamas, Douglas, Grant, Jefferson, Lane, Linn, Marion, Morrow, Umatilla, Union, Wallowa, Wheeler. LEGAL - Not Applicable. Order will apply to all Forests in Region 6, however targeted scoping is with the Umatilla, Gifford Pinchot, Mt. Baker/Snoqualmie, Willamette and Colville NFs tribal and public scoping lists. Mt Baker-Snoqualmie National Forest, Forestwide (excluding Projects occurring in more than one Forest) R6 - Pacific Northwest Region Invasive Plant Management - Vegetation management In Progress: Expected:04/2015 05/2015 Phyllis Reed EIS (other than forest products) NOI in Federal Register 360-436-2332 02/28/2012 [email protected] Est. -
Mt Baker-Snoqualmie National Forest EA CE
Schedule of Proposed Action (SOPA) 07/01/2007 to 09/30/2007 Mt Baker-Snoqualmie National Forest This report contains the best available information at the time of publication. Questions may be directed to the Project Contact. Expected Project Name Project Purpose Planning Status Decision Implementation Project Contact Projects Occurring Nationwide Aerial Application of Fire - Fuels management In Progress: Expected:08/2007 08/2007 Christopher Wehrli Retardant 215 Comment Period Legal 202-205-1332 EA Notice 07/28/2006 [email protected] Description: The Forest Service proposes to continue the aerial application of fire retardant to fight fires on National Forest System lands. An environmental analysis will be conducted to prepare an Environmental Assessment on the proposed action. Web Link: http://www.fs.fed.us/fire/retardant/index.html Location: UNIT - All Districts-level Units. STATE - All States. COUNTY - All Counties. Nation Wide. R6 - Pacific Northwest Region, Occurring in more than one Forest (excluding Regionwide) Aquatic Outfitter and Guide - Special use management Developing Proposal Expected:08/2008 01/2009 Don Gay Special Use Permits Est. Scoping Start 11/2007 360-856-5700 CE [email protected] Description: Issuance of special use permits for outfitter and guides using the N.F. Nooksack, Skagit, Sauk, Skykomish, and Cispus Rivers. Location: UNIT - Mt Baker Ranger District, Darrington Ranger District, Skykomish Ranger District, Cowlitz Ranger District. STATE - Washington. COUNTY - Lewis, Skagit, Snohomish, Whatcom. LEGAL - T40NR6E, T39NR6 and 7E, T39NR7E, T35NR8,9,10E, T36NR11E, T31-35NR10E, T32NR9E, T27NR9 and 10E, T11NR5,6,7, and 8E. N. F. Nooksack, Skagit, Sauk, Skykomish, and Cispus Rivers. -
Yakama-Cowlitz Trail: Ancient and Modern Paths Across the Mountains
COLUMBIA THE MAGAZINE OF NORTHWEST HISTORY ■ SUMMER 2018 Yakama-Cowlitz Trail: Ancient and modern paths across the mountains North Cascades National Park celebrates 50 years • Explore WPA Legacies A quarterly publication of the Washington State Historical Society TWO CENTURIES OF GLASS 19 • JULY 14–DECEMBER 6, 2018 27 − Experience the beauty of transformed materials • − Explore innovative reuse from across WA − See dozens of unique objects created by upcycling, downcycling, recycling − Learn about enterprising makers in our region 18 – 1 • 8 • 9 WASHINGTON STATE HISTORY MUSEUM 1911 Pacific Avenue, Tacoma | 1-888-BE-THERE WashingtonHistory.org CONTENTS COLUMBIA The Magazine of Northwest History A quarterly publication of the VOLUME THIRTY-TWO, NUMBER TWO ■ Feliks Banel, Editor Theresa Cummins, Graphic Designer FOUNDING EDITOR COVER STORY John McClelland Jr. (1915–2010) ■ 4 The Yakama-Cowlitz Trail by Judy Bentley OFFICERS Judy Bentley searches the landscape, memories, old photos—and President: Larry Kopp, Tacoma occasionally, signage along the trail—to help tell the story of an Vice President: Ryan Pennington, Woodinville ancient footpath over the Cascades. Treasurer: Alex McGregor, Colfax Secretary/WSHS Director: Jennifer Kilmer EX OFFICIO TRUSTEES Jay Inslee, Governor Chris Reykdal, Superintendent of Public Instruction Kim Wyman, Secretary of State BOARD OF TRUSTEES Sally Barline, Lakewood Natalie Bowman, Tacoma Enrique Cerna, Seattle Senator Jeannie Darneille, Tacoma David Devine, Tacoma 14 Crown Jewel Wilderness of the North Cascades by Lauren Danner Suzie Dicks, Belfair Lauren14 Danner commemorates the 50th22 anniversary of one of John B. Dimmer, Tacoma Washington’s most special places in an excerpt from her book, Jim Garrison, Mount Vernon Representative Zack Hudgins, Tukwila Crown Jewel Wilderness: Creating North Cascades National Park. -
Mapping of Major Latest Pleistocene to Holocene Eruptive Episodes from the Glacier Peak Volcano, Washington—A Record of Lahar
MAPPING OF MAJOR LATEST PLEISTOCENE TO HOLOCENE ERUPTIVE EPISODES FROM THE GLACIER PEAK VOLCANO, WASHINGTON—A RECORD OF LAHARIC INUNDATION OF THE PUGET LOWLANDS FROM DARRINGTON TO THE PUGET SOUND 123° 122° 121° 49° Benjamin W. Stanton and Joe D. Dragovich, Washington Department of Natural Resouces, Division of Geology and Earth Resources, 1111 Washington St SE, Olympia, WA 98504-7007, [email protected] and [email protected] map area Bellingham SAN WHA TCOM 20 JUAN Volcanic hazards in the Pacific Northwest are typically associated with more visible stratovolcanoes, such as Mount Rainier. Glacier Peak, a North Cascade dacitic stratovolcano near Darrington, Washington, has produced at least three large eruptive episodes See Figure 2 14 path of lahars since the culmination of the last continental glaciation with each episode likely lasting a few hundred years. Data from recent detailed geologic mapping, new C ages, stratigraphic relations, clast petrographic analyses, geochemical analyses, and laharic SKAGIT to lower Skagit Valley ISLAND sand composition indicate that three large eruptive episodes occurred in the latest Pleistocene and Holocene—the information refines and expands on the pioneering work of Beget (1981). These voluminous events traveled up to 135 km downvalley of the path of lahars to lower Stillaguamish Valley Glacier Peak edifice and reached the Puget Sound via the ancient Skagit and Stillaguamish deltas. Glacier Peak has erupted dacite of similar composition throughout its history. Hypersthene-hornblende-(augite)-phyric vesicular lahar clasts found from Glacier Peak to La volcano 48° SNOHMISH Conner, Washington have similar geochemistry to dacite flows sampled on the volcano. Radiocarbon dating of the White Chuck assemblage shows an eruptive episode of ~11,900 yrs B.P. -
Biological Evaluation
BIOLOGICAL EVALUATION SKAGIT RIVER HYDROELECTRIC PROJECT LICENSE (FERC NO. 553) AMENDMENT: ADDITION OF A SECOND POWER TUNNEL AT THE GORGE DEVELOPMENT Final June 2011 BIOLOGICAL EVALUATION Table of Contents 1 INTRODUCTION .................................................................................................................. 1 1.1. Project Location .........................................................................................................2 1.2. Summary of Skagit River Project History ..................................................................2 1.2.1. Project Construction and Original License ................................................... 2 1.2.2. Settlement Agreement and Current License .................................................. 2 2 EXISTING PROJECT FACILITIES, OPERATIONS, AND MITIGATION AND CONSERVATION MEASURES ........................................................................................... 6 2.1. Existing Project Facilities ...........................................................................................6 2.1.1. Project Developments ................................................................................... 6 2.1.2. Diablo and Newhalem ................................................................................... 7 2.1.3. Project Transmission Lines ........................................................................... 7 2.2. Existing Operations – Reservoirs ...............................................................................8 2.2.1. Ross Lake -
Puget Sound Salmon Habitat Assessment: Landscape Level Subwatershed Prioritization
CONSERVATION PRIORITIES: AN ASSESSMENT OF FRESHWATER HABITAT FOR PUGET SOUND SALMON PREFACE This report entitled Conservation Priorities: An assessment of freshwater habitat for Puget Sound Salmon was prepared at the request of the Trust for Public Land (TPL) to provide a regional snapshot of Puget Sound’s most pristine, intact freshwater salmon habitat. TPL is a leading land conservation organization whose mission includes conserving land for people which often means protecting habitat critical to the health of salmon and other species. We believe the assessment can complement and enhance the work of many organizations that are striving to recover our Puget Sound salmon runs. The assessment is a synthesis of existing information and expert opinion. The report describes or attempts to draw from what is known, published and described by experts within agencies, tribes and watershed groups having direct knowledge of these ecosystems and populations. The assessment provides a priority listing and map of the most intact freshwater habitats for salmon in the Puget Sound. The prioritized list of habitats, together with the summarized information and compiled sources, can be used to help guide cost- effective conservation decision making in the near term for the benefit of salmon and encompasses the whole Puget Sound basin. Dr. Chris Frissell, of the Flathead Lake Biological Station at the University of Montana; Peter Morrison, Pacific Biodiversity Institute; Jim Kramer, natural resource consultant; and Marie Mentor, a consultant and former TPL Washington State Director, were retained to produce the assessment. This effort would not have been possible without the significant support provided by The Brainerd Foundation, the Kongsgaard-Goldman Foundation, King County, the Bullitt Foundation, and in-kind contributions from Pacific Biodiversity Institute and TPL. -
Glacier Peak — History and Hazards of a Cascade Volcano
USG S U.S. GEOLOGICAL SURVEY — REDUCING RISK FROM VOLCANO HAZARDS Glacier Peak — History and Hazards of a Cascade Volcano lacier Peak is the most Gremote of the five active volcanoes in Washington State. It is not prominently visible from any major popu- lation center, and so its attractions, as well as its hazards, tend to be over- looked. Yet since the end of the last ice age, Glacier Peak has produced some of the largest and most explosive eruptions in the state. During this time period, Glacier Peak has erupted multiple times during at least six separate Baker episodes, most recently Pacific Ocean about 300 years ago. What Glacier Peak lies in Washington State’s North Cascade Mountains, were these eruptions like? Glacier in the heart of a wilderness area bearing its name. Its past Peak Could similar ones affect us eruptions have melted snow and ice to inundate downstream today? Scientists from the valleys with rocks, mud, and debris. Large eruptions from Glacier Rainier U.S. Geological Survey Peak have deposited ash throughout much of the western United St. Helens States and southwestern Canada. Photo by D.R. Mullineaux, USGS. Adams (USGS) are working to WASHINGTON answer these questions and Glacier Peak lies only 70 miles help prepare for future northeast of Seattle—closer to that city activity. than any volcano except Mount Rainier. Since the continental ice sheets receded But unlike Mount Rainier, it rises only a from the region, Glacier Peak has erupted The stunning snow-capped volcanoes few thousand feet above neighboring repeatedly during at least six episodes. -
GEOLOGIC HISTORY of SKAGIT VALLEY Years Ago Volcano Event
GEOLOGIC HISTORY OF SKAGIT VALLEY Years Ago Volcano Event 6,000,000 Cascade Mountain range began to uplift.8 2,000,000 Northern Washington was buried by several continental ice sheets.8 14,000 GP Oldest known deposits are in the White Chuck River Valley.1 Glaciers began retreating.10 SOURCES: 1. Postglacial Volcanic Deposits at Glacier Peak, Washington, and Potential Hazards from Future Eruptions, by James E. Beget, (1982, Open File Report 82-830 Glacier Peak 2. Soil survey TransMountain pipeline (1989). 3. Prehistoric Settlement Changes in the Southern Northwest Coast: A Functional Approach, by Gail Thompson, Ph.D.., (1978), Geological Survey Professional Paper 1022C 4. Postglacial Volcanic Deposits at Mt.. Baker, Washington, and Potential Hazards from Future Eruptions, by Jack Hyde & Dwight Crandell, (1978), Geological Survey Professional Paper 1022C 5. Increased Heat Emission From Mount Baker, WA., by Stephen Malone & David Frank (Post 1975) 6. From the Mountains to the Sea, by Saul Weisberg & John Riedel, (1991) 7. Fire and Ice, The Cascade Volcanoes, Stephen L. Harris, (1976) 8. Northwest Volcanoes, A Roadside Geologic Guide, Lanny Ream, (1983) 9. Sleeping Beauty, by Charles Siderius, Skagit Valley Herald (1991) 10. Recent Volcanic Activity at Glacier Peak, James E. Beget, (1982), Science Vol.. 215 11. Fire Mountains Of The West, Stephen L. Harris 1 GEOLOGIC HISTORY OF SKAGIT VALLEY Years Ago Volcano Event 13,000 Sea level was 600 ft above present location. Deposition of estuarine and deltaic sediments began. Discharge of sediment materials would have begun around Hamilton.3 12,000 GP Violent eruption depositing widespread layers of ash.7 12-11,000 Sea level drops rapidly and becomes relatively stable.3 SOURCES: 1. -
This Report Is Preliminary and Has Not Been Reviewed for Conformity with U.S
UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY ANNOTATED GUIDE TO GEOLOGIC REPORTS AND MAPS OF THE GLACIER PEAK WILDERNESS AND ADJACENT AREAS, NORTHERN CASCADES, WASHINGTON By Arthur B. Ford Open-File Report 83-97 1983 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards and strati graphic nomenclature. CONTENTS Page Introduction 1 Acknowledgments 1 Miscellaneous topics 6 Glacier Peak volcano, volcanism, and thermal springs 7 Quaternary geology and glacier studies 11 Regional geology and geologic setting 14 Bedrock geology and petrology of the wilderness area 18 Geochronology and isotope studies 24 Geophysical studies 27 Mineral deposits and resource studies 28 ILLUSTRATIONS Figure 1. Location of the Glacier Peak Wilderness 2 Figure 2. Index to geologic mapping in and near the Glacier Peak Wilderness 3 Figure 3. Index to topographic map quadrangles of the Glacier Peak Wilderness and vicinity -- 5 INTRODUCTION This listing of reports and maps related to the geology, mineral resources, and other aspects of the Glacier Peak Wilderness and vicinity in the northern Cascade Mountains of Washington (fi<j. 1) was prepared as a background for 1979-82 field studies on the geol >gy (Ford and others, 1983), regional geophysics (Flanigan and Sherrard, 1983), and geochemistry (Church and others, 1983) of the Wilderness by the U.S. Geological Survey. The studies were part of an investigation of the mineral-resource potential of the Wilderness by the Survey and the U.S. Bureau of Mines, results of which are given, by Church and others (in press) and summarized by Church and Stotelmeyer (in press). -
Reconstruction of the North Sauk River Road Snohomish County, WA FEMA-1499-DR-WA (Public Assistance) August 2006
Environmental Assessment Reconstruction of the North Sauk River Road Snohomish County, WA FEMA-1499-DR-WA (Public Assistance) August 2006 U.S. Department of Homeland Security FEMA Region X 130 228th Street SW Bothell, WA 98021-9796 Environmental Assessment for FEMA Reconstruction of the North Sauk River Road TABLE OF CONTENTS FONSI.....................................................................................................................FONSI-1 1.0 PURPOSE AND NEED FOR ACTION.......................................................................1 1.1 Introduction.......................................................................................................1 1.2 Purpose and Need for Action............................................................................1 1.3 Location and Background.................................................................................1 2.0 ALTERNATIVES.........................................................................................................5 2.1 Alternatives Analyzed in this EA .....................................................................5 2.1.1 Alternative A – No Action Alternative..............................................5 2.1.2 Alternative B – East Alignment with Low Walls ..............................5 2.1.3 Alternative C – DNR Road................................................................6 2.1.4 Alternative D – Modified DNR Road (Preferred Alternative) ..........6 2.2 Alternatives Considered But Not Carried Forward ..........................................7