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North Cascades Contested Terrain
North Cascades NP: Contested Terrain: North Cascades National Park Service Complex: An Administrative History NORTH CASCADES Contested Terrain North Cascades National Park Service Complex: An Administrative History CONTESTED TERRAIN: North Cascades National Park Service Complex, Washington An Administrative History By David Louter 1998 National Park Service Seattle, Washington TABLE OF CONTENTS adhi/index.htm Last Updated: 14-Apr-1999 http://www.nps.gov/history/history/online_books/noca/adhi/[11/22/2013 1:57:33 PM] North Cascades NP: Contested Terrain: North Cascades National Park Service Complex: An Administrative History (Table of Contents) NORTH CASCADES Contested Terrain North Cascades National Park Service Complex: An Administrative History TABLE OF CONTENTS Cover Cover: The Southern Pickett Range, 1963. (Courtesy of North Cascades National Park) Introduction Part I A Wilderness Park (1890s to 1968) Chapter 1 Contested Terrain: The Establishment of North Cascades National Park Part II The Making of a New Park (1968 to 1978) Chapter 2 Administration Chapter 3 Visitor Use and Development Chapter 4 Concessions Chapter 5 Wilderness Proposals and Backcountry Management Chapter 6 Research and Resource Management Chapter 7 Dam Dilemma: North Cascades National Park and the High Ross Dam Controversy Chapter 8 Stehekin: Land of Freedom and Want Part III The Wilderness Park Ideal and the Challenge of Traditional Park Management (1978 to 1998) Chapter 9 Administration Chapter 10 http://www.nps.gov/history/history/online_books/noca/adhi/contents.htm[11/22/2013 -
OFR 2019–1144: Preliminary Assessment of Shallow Groundwater Chemistry Near Goodell Creek, North Cascades National Park, Washi
Prepared in cooperation with the National Park Service Preliminary Assessment of Shallow Groundwater Chemistry near Goodell Creek, North Cascades National Park, Washington Open-File Report 2019–1144 U.S. Department of the Interior U.S. Geological Survey Preliminary Assessment of Shallow Groundwater Chemistry near Goodell Creek, North Cascades National Park, Washington By Rich W. Sheibley and James R. Foreman Prepared in cooperation with the National Park Service Open-File Report 2019–1144 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior David Bernhardt, Secretary U.S. Geological Survey James F. Reilly II, Director U.S. Geological Survey, Reston, Virginia: 2019 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment—visit https://www.usgs.gov/ or call 1–888–ASK–USGS (1–888–275–8747). For an overview of USGS information products, including maps, imagery, and publications, visit https://store.usgs.gov/. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this information product, for the most part, is in the public domain, it also may contain copyrighted materials as noted in the text. Permission to reproduce copyrighted items must be secured from the copyright owner. Suggested citation: Sheibley, R.W., and Foreman, J.R., 2019, Preliminary assessment of shallow groundwater chemistry near Goodell Creek, North Cascades National Park, Washington: U.S. Geological Survey Open-File Report 2019–1144, 14 p., https://doi.org/10.3133/ofr20191144. -
Stratigraphy, Age, and Provenance of the Eocene Chumstick Basin
Stratigraphy, age, and provenance of the Eocene Chumstick basin, Washington Cascades; implications for paleogeography, regional tectonics, and development of strike-slip basins Erin E. Donaghy1,†, Paul J. Umhoefer2, Michael P. Eddy1, Robert B. Miller3, and Taylor LaCasse4 1 Department of Earth, Planetary, and Atmospheric Sciences, Purdue University, West Lafayette, Indiana 47907, USA 2 School of Earth Sciences and Sustainability, Northern Arizona University, Flagstaff, Arizona 86011, USA 3 Department of Geology, San Jose State University, San Jose, California 95192, USA 4 Department of Geology, Carleton College, Northfield, Minnesota 55057 USA ABSTRACT tions can be constrained at high temporal Here we present a large provenance data set resolution (0.5–1.5 m.y. scale) for an ancient coupled with new lithofacies mapping from Strike-slip faults form in a wide variety strike-slip basin and permits a detailed re- the Chumstick basin within the framework of a of tectonic settings and are a first-order construction of sediment routing pathways recently developed precise depositional chronol- control on the geometry and sediment accu- and depositional environments. As a result, ogy (Eddy et al., 2016b). This basin formed in mulation patterns in adjacent sedimentary we can assess how varying sediment supply a strike-slip setting in central Washington and basins. Although the structural and depo- and accommodation space affects the depo- provides a unique opportunity to track changes sitional architecture of strike-slip basins is sitional architecture during strike-slip basin in sediment routing systems that are related well documented, few studies of strike-slip evolution. to rapidly changing paleogeography in basin- basins have integrated depositional age, bounding basement blocks. -
Where the Water Meets the Land: Between Culture and History in Upper Skagit Aboriginal Territory
Where the Water Meets the Land: Between Culture and History in Upper Skagit Aboriginal Territory by Molly Sue Malone B.A., Dartmouth College, 2005 A THESIS SUBMITTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF PHILOSOPHY in The Faculty of Graduate and Postdoctoral Studies (Anthropology) THE UNIVERSITY OF BRITISH COLUMBIA (Vancouver) December 2013 © Molly Sue Malone, 2013 Abstract Upper Skagit Indian Tribe are a Coast Salish fishing community in western Washington, USA, who face the challenge of remaining culturally distinct while fitting into the socioeconomic expectations of American society, all while asserting their rights to access their aboriginal territory. This dissertation asks a twofold research question: How do Upper Skagit people interact with and experience the aquatic environment of their aboriginal territory, and how do their experiences with colonization and their cultural practices weave together to form a historical consciousness that orients them to their lands and waters and the wider world? Based on data from three methods of inquiry—interviews, participant observation, and archival research—collected over sixteen months of fieldwork on the Upper Skagit reservation in Sedro-Woolley, WA, I answer this question with an ethnography of the interplay between culture, history, and the land and waterscape that comprise Upper Skagit aboriginal territory. This interplay is the process of historical consciousness, which is neither singular nor sedentary, but rather an understanding of a world in flux made up of both conscious and unconscious thoughts that shape behavior. I conclude that the ways in which Upper Skagit people interact with what I call the waterscape of their aboriginal territory is one of their major distinctive features as a group. -
Upper Skagit
A GUIDE TO PEOPLE AND PLACES OF THE UPPER SKAGIT BOB MIERENDORF AND GERRY COOK NORTH CASCADES NATIONAL PARK SERVICE COMPLEX NORTH CASCADES INSTITUTE JULY 22–25 2010 1 CLASS FIELD DAYS ITINERARY PEOPLE AND PLACES OF THE UPPER SKAGIT RIVER JULY 22–25, 2010 FRIDAY 9 am Drive from ELC to Ross Dam Trailhead parking lot 9:15–10:00 Hike to Ross Lake (end of haul road) – Brief stop on trail at a Ross Dam overlook – Load ourselves and gear on the Mule 10:30 am Welcome to the Wild Upper Skagit – Rules of the Mule and other safety matters – Instructor and participant introductions Noon Lunch on the Mule near Big Beaver Creek 2:45 pm Second stop near May Creek (no rest rooms here) 6 pm Arrive at Lightning Horse Camp (our base camp for two nights) 7 pm Potluck dinner SATURDAY 7 am Breakfast 8 am–Noon Ethnobotany hike along Eastbank Trail – About a two mile hike, rolling terrain – Gerry will pick us up with the Mule – Lunch on the Mule 1 pm Quick rest room stop at Boundary Bay Campground 3 pm Arrive at International Boundary 3:15 pm Stop at Winnebago Flats – There are toilets here – Get drinking water and fill water jugs 3:45 pm Depart Winnebago Flats on return trip 5 pm Arrive back at our camp 6:30 pm Potluck dinner SUNDAY ABOUT THE COVER 7 am Breakfast U.S. Forest Service, Mt. Baker 8 am Break camp and load Mule Ranger District, 1931 oblique 9 am Depart on Mule aerial facing 182o (south), of pre-impoundment Skagit River 10 am Arrive at Big Beaver Campground flood plain; Skymo Creek canyon – There are rest rooms here in lower right, Devil’s Creek canyon – Hike up Big Beaver to old growth cedar grove emerging from middle left. -
Soil Survey of North Cascades National Park Complex, Washington
UNITED STATES DEPARTMENT OF THE INTERIOR NATIONAL PARK SERVICE SOIL SURVEY OF NORTH CASCADES Joins sheet 11, Mount Prophet NATIONAL PARK COMPLEX, WASHINGTON UNITED STATES DEPARTMENT OF AGRICULTURE ROSS DAM QUADRANGLE NATURAL RESOURCES CONSERVATION SERVICE SHEET NUMBER 18 OF 34 121°7’30"W 121°5’0"W Joins sheet 12, Pumpkin Mountain 121°2’30"W 121°0’0"W Joins sheet 13, Jack Mountain 8006 6502 9001 9010 9003 9003 7502 9003 9012 7015 6015 9999 48°45’0"N Sourdough Mountain 48°45’0"N 9010 9016 TRAIL 9008 7502 6014 9001 9003 7501 TRAIL 8007 9003 9003 9010 SOURDOUGH 9010 7015 9016 6010 7502 9016 9997 TRAIL 6505 9010 9008 6014 BEAVER 7502 9003 BANK BIG 9008 MOUNTAIN Hidden Hand 9016 Pass TRAIL 6010 9012 7501 9999 9003 9012 7502 ROSS LAKE 9010 7003 EAST NATIONAL RECREATION AREA BOUNDARY 7501 LAKE ROSS MOUNTAIN ROSS 7015 NORTH CASCADES NATIONAL PARK BOUNDARY DAM 9997 9016 7502 7501 Ruby Arm 6015 9001 7502 7015 6015 6009 7003 7015 9016 7500 9003 Happy JACK 6009 9999 7003 7502 7501 NORTH CASCADES HIGHWAY ( closed mid-Nov to April ) 9999 7501 6015 6014 Creek Diablo Lake DIABLO 6014 7502 Resort 7501 9997 TRAIL 6014 7015 7501 7015 9997 LAKE 6014 7003 7003 20 9999 7015 6009 7015 7015 7003 9999 DIABLO LAKE 6010 20 7003 6014 9016 48°42’30"N 9003 48°42’30"N 20 6014 6015 7015 9016 7003 6015 9012 6014 9012 7015 7015 9012 9012 NORTH CASCADES HIGHWAY 9016 7015 9003 THUNDER 7502 9010 7015 7501 9016 Thunder 9010 6015 7003 Lake KNOB 7501 7015 9999 9012 Pyramid 7015 6014 Lake Ruby 7003 9998 Mountain TRAIL Thunder Arm 9012 8006 9003 9012 7502 6014 9010 7015 6014 9012 -
Skagit - Ferc Project #553
SKAGIT - FERC PROJECT #553 EROSION CONTROL PROGRAM 2005 COMPLETION REPORT North Cascades National Park and Seattle City Light March, 2006 1 INTRODUCTION As stipulated in the 1991 Erosion Control Settlement Agreement (SA) between the National Park Service (NPS) and Seattle City Light (SCL), erosion control activities in Ross Lake National Recreation Area (NRA) continued for a twelfth year (including pre-license work). NPS crews, funded by SCL, conducted work at several sites in 2005 (Figure 1). Activity this year focused on contingency cribbing site E70A-6B, twenty yards south of E70A-6 on Ross Lake. In addition, site D-11, Thunder Point Campground on Diablo Lake was undertaken and completed. Detailed accounting of expenditures is provided in other reports and is not duplicated here. The purpose of this report is to update the Federal Energy Regulatory Commission (FERC) on progress under the terms of the new operating license for the Skagit Project. PROGRESS REPORTS BY PROJECT SITE D-11, Diablo Lake: Thunder Point Campground Approximately 250 ft of shoreline fronting the campground had become severely eroded. NPS erosion control crews in coordination with Seattle City Light barge, tug and boat crew imported 23 dump truck loads of building rock and one hundred yards of gravel. As per settlement agreement erosion control design, dry lay rock wall was installed to a height of 5’ along the 250’ of shoreline. Upon completion of dry wall, armor rock placed along the toe for the entire span. On the southwest end of the site, an additional 60’ of eroded shoreline was protected by half burying stumps in the drawdown and locking in drift logs in between the buried stumps and the shoreline creating a wave energy break. -
1934 the MOUNTAINEERS Incorpora.Ted T�E MOUNTAINEER VOLUME TWENTY-SEVEN Number One
THE MOUNTAINEER VOLUME TWENTY -SEVEN Nom1-0ae Deceml.er, 19.34 GOING TO GLACIER PUBLISHED BY THE MOUNTAIN�ER.S INCOaPOllATBD SEATTLI: WASHINGTON. _,. Copyright 1934 THE MOUNTAINEERS Incorpora.ted T�e MOUNTAINEER VOLUME TWENTY-SEVEN Number One December, 1934 GOING TO GLACIER 7 •Organized 1906 Incorporated 1913 EDITORIAL BOARD, 1934 Phyllis Young Katharine A. Anderson C. F. Todd Marjorie Gregg Arthur R. Winder Subscription Price, $2.00 a Year Annual (only) Seventy-five Cents Published by THE MOUNTAINEERS Incorporated Seattle, Washington Entered as second class matter, December 15, 1920, at the Postofflce at Seattle, Washington, under the Act of March 3, 1879. TABLE OF CONTENTS Greeting ........................................................................Henr y S. Han, Jr. North Face of Mount Rainier ................................................ Wolf Baiter 3 r Going to Glacier, Illustrated ............... -.................... .Har iet K. Walker 6 Members of the 1934 Summer Outing........................................................ 8 The Lake Chelan Region ............. .N. W. <J1·igg and Arthiir R. Winder 11 Map and Illustration The Climb of Foraker, Illitstrated.................................... <J. S. Houston 17 Ascent of Spire Peak ............................................... -.. .Kenneth Chapman 18 Paradise to White River Camp on Skis .......................... Otto P. Strizek 20 Glacier Recession Studies ................................................H. Strandberg 22 The Mounta,ineer Climbers................................................ -
Washington State's Scenic Byways & Road Trips
waShington State’S Scenic BywayS & Road tRipS inSide: Road Maps & Scenic drives planning tips points of interest 2 taBLe of contentS waShington State’S Scenic BywayS & Road tRipS introduction 3 Washington State’s Scenic Byways & Road Trips guide has been made possible State Map overview of Scenic Byways 4 through funding from the Federal Highway Administration’s National Scenic Byways Program, Washington State Department of Transportation and aLL aMeRican RoadS Washington State Tourism. waShington State depaRtMent of coMMeRce Chinook Pass Scenic Byway 9 director, Rogers Weed International Selkirk Loop 15 waShington State touRiSM executive director, Marsha Massey nationaL Scenic BywayS Marketing Manager, Betsy Gabel product development Manager, Michelle Campbell Coulee Corridor 21 waShington State depaRtMent of tRanSpoRtation Mountains to Sound Greenway 25 Secretary of transportation, Paula Hammond director, highways and Local programs, Kathleen Davis Stevens Pass Greenway 29 Scenic Byways coordinator, Ed Spilker Strait of Juan de Fuca - Highway 112 33 Byway leaders and an interagency advisory group with representatives from the White Pass Scenic Byway 37 Washington State Department of Transportation, Washington State Department of Agriculture, Washington State Department of Fish & Wildlife, Washington State Tourism, Washington State Parks and Recreation Commission and State Scenic BywayS Audubon Washington were also instrumental in the creation of this guide. Cape Flattery Tribal Scenic Byway 40 puBLiShing SeRviceS pRovided By deStination -
1976 Bicentennial Mckinley South Buttress Expedition
THE MOUNTAINEER • Cover:Mowich Glacier Art Wolfe The Mountaineer EDITORIAL COMMITTEE Verna Ness, Editor; Herb Belanger, Don Brooks, Garth Ferber. Trudi Ferber, Bill French, Jr., Christa Lewis, Mariann Schmitt, Paul Seeman, Loretta Slater, Roseanne Stukel, Mary Jane Ware. Writing, graphics and photographs should be submitted to the Annual Editor, The Mountaineer, at the address below, before January 15, 1978 for consideration. Photographs should be black and white prints, at least 5 x 7 inches, with caption and photo grapher's name on back. Manuscripts should be typed double· spaced, with at least 1 Y:z inch margins, and include writer's name, address and phone number. Graphics should have caption and artist's name on back. Manuscripts cannot be returned. Properly identified photographs and graphics will be returnedabout June. Copyright © 1977, The Mountaineers. Entered as second·class matter April8, 1922, at Post Office, Seattle, Washington, under the act of March 3, 1879. Published monthly, except July, when semi-monthly, by The Mountaineers, 719 Pike Street,Seattle, Washington 98101. Subscription price, monthly bulletin and annual, $6.00 per year. ISBN 0-916890-52-X 2 THE MOUNTAINEERS PURPOSES To explore and study the mountains, forests, and watercourses of the Northwest; To gather into permanentform the history and tra ditions of thisregion; To preserve by the encouragement of protective legislation or otherwise the natural beauty of NorthwestAmerica; To make expeditions into these regions in fulfill ment of the above purposes; To encourage a spirit of good fellowship among all loversof outdoor life. 0 � . �·' ' :···_I·:_ Red Heather ' J BJ. Packard 3 The Mountaineer At FerryBasin B. -
Preliminary Geologic Map of the Mount Baker 30- by 60-Minute Quadrangle, Washington
U.S. DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY Preliminary Geologic Map of the Mount Baker 30- by 60-Minute Quadrangle, Washington by R.W. Tabor1 , R.A. Haugerud2, D.B. Booth3, and E.H. Brown4 Prepared in cooperation with the Washington State Department of Natural Resources, Division of Geology and Earth Resources, Olympia, Washington, 98504 OPEN FILE REPORT 94-403 This report is preliminary and has not been reviewed for conformity with U.S.Geological Survey editorial standards or with the North American Stratigraphic Code. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government. iu.S.G.S., Menlo Park, California 94025 2U.S.G.S., University of Washington, AJ-20, Seattle, Washington 98195 3SWMD, King County Department of Public Works, Seattle, Washington, 98104 ^Department of Geology, Western Washington University, Bellingham, Washington 98225 INTRODUCTION The Mount Baker 30- by 60-minute quadrangle encompasses rocks and structures that represent the essence of North Cascade geology. The quadrangle is mostly rugged and remote and includes much of the North Cascade National Park and several dedicated Wilderness areas managed by the U.S. Forest Service. Geologic exploration has been slow and difficult. In 1858 George Gibbs (1874) ascended the Skagit River part way to begin the geographic and geologic exploration of the North Cascades. In 1901, Reginald Daly (1912) surveyed the 49th parallel along the Canadian side of the border, and George Smith and Frank Calkins (1904) surveyed the United States' side. Daly's exhaustive report was the first attempt to synthesize what has become an extremely complicated geologic story. -
Geologic Map of the North Cascade Range, Washington by Ralph A
Prepared in cooperation with Washington State Division of Geology and Earth Resources, U.S. National Park Service, and U.S. Forest Service Geologic Map of the North Cascade Range, Washington By Ralph A. Haugerud and Rowland W. Tabor Nontechnical pamphlet to accompany Scientific Investigations Map 2940 Looking south from the North Klawatti Glacier [Mbse]. In the right foreground, the glacier breaks into a heavily crevassed icefall where it descends steeply. Rock in the foreground knob is Eldorado Orthogneiss (unit TKgo), a 90 million-year-old stitching pluton, which here includes numerous dikes of light- colored pegmatite. Mount Buckner on the left skyline and Mount Forbidden hidden in clouds are also eroded from the Eldorado Orthogneiss (photographed in 1987). 2009 U.S. Department of the Interior U.S. Geological Survey CONTENTS Introduction.....................................................................................................................................................1 Using this report ....................................................................................................................................1 Map preparation ...................................................................................................................................1 Major sources of new data .................................................................................................................1 Acknowledgments ................................................................................................................................2