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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 -
Cascades Butterfly Project North Cascades National Park Resource Brief - 2011
CASCADES BUTTERFLY PROJECT NORTH CASCADES NATIONAL PARK RESOURCE BRIEF - 2011 Cascades Butterfly Project Climate change is expected to affect mountain ecosystems in many ways. Scientists predict that warmer summers may result in earlier snowmelt, more frequent forest fires, and changes in distributions of plants and animals. Although some ecosystem changes have already been observed, (e.g. melting glaciers), many future impacts remain uncertain. Monitoring provides a way to document ecosystem changes, anticipate future changes, and improve management of protected lands. Butterflies are sensitive indicators of butterflies are able to fly to higher eleva- climate change because temperature tions in response to warming tempera- influences the timing of an individual’s tures, will they be able to establish as life cycle and the geographic distribu- breeding residents? Will host plants be tion of species. As individuals develop able to migrate up quickly enough to from egg to larvae to pupae and finally support butterfly populations, or will to mature butterfly, temperature thresh- some species become extinct? olds may trigger these changes. Annual temperature patterns are often the What are we doing? primary determinant of the distribution Six protected areas in the Cascade of “generalist” butterflies. Generalist Mountains are establishing a program butterflies are species that can utilize to monitor butterflies to learn how cli- many different plant species for nectar, mate is affecting their populations. The larval development, and egg deposition. six areas include four sites in Washing- Specialist butterflies depend on a few ton: North Cascades National Park, plant species for food and development Mount Baker-Snoqualmie National and they can be directly and indirectly Forest, Okanagan-Wenatchee National influenced by climate (temperature and Forest, and Mount Rainier National precipitation). -
Stehekin River Classification
Stehekin Wild & Scenic River Eligibility Report FINAL DRAFT May 2002 Acknowledgments . The National Park Service gratefully acknowledges the support and assistance of the U.S. Forest Service Wenatchee and Okanogan National Forests – their assistance was critical in this report’s development. Special thanks also to the staff at the North Cascades National Park for helping to make the field work a very pleasant and informative experience. Executive Summary This study report evaluates the eligibility and classification of the Stehekin River watershed, located in the North Cascades Mountains of Washington State, as a component of the National Wild and Scenic Rivers System (National System). This evaluation is done partially in settlement of a cause of action brought by the North Cascades Conservation Council1, but primarily as a Department of the Interior requirement for normal management planning processes. The Stehekin River and its tributaries constitute a comparatively small watershed. Most of the natural and cultural resources found in the watershed are dependent not just on the main stem of the Stehekin River, but also on its tributaries. There is also no clear demarcation between most resources throughout the watershed. For these reasons, it is appropriate to consider the entire Stehekin River system as a single unit for the purposes of this evaluation, with the exception of classifying segments of the river as described later. Under the Wild and Scenic Rivers Act (Act), the river must meet physical requirements (eligibility). These physical requirements are: 1) the river must be free-flowing; and 2) the river must have at least one resource important or unique to the region or nation. -
The Wild Cascades
THE WILD CASCADES October-November 1969 2 THE WILD CASCADES FARTHEST EAST: CHOPAKA MOUNTAIN Field Notes of an N3C Reconnaissance State of Washington, school lands managed by May 1969 the Department of Natural Resources. The absolute easternmost peak of the North Cascades is Chopaka Mountain, 7882 feet. An This probably is the most spectacular chunk abrupt and impressive 6700-foot scarp drops of alpine terrain owned by the state. Certain from the flowery summit to blue waters of ly its fame will soon spread far beyond the Palmer Lake and meanders of the Similka- Okanogan. Certainly the state should take a mean River, surrounded by green pastures new, close look at Chopaka and develop a re and orchards. Beyond, across this wide vised management plan that takes into account trough of a Pleistocene glacier, roll brown the scenic and recreational resources. hills of the Okanogan Highlands. Northward are distant, snowy beginnings of Canadian ranges. Far south, Tiffany Mountain stands above forested branches of Toats Coulee Our gang became aware of Chopaka on the Creek. Close to the west is the Pasayten Fourth of July weekend of 1968 while explor Wilderness Area, dominated here by Windy ing Horseshoe Basin -- now protected (except Peak, Horseshoe Mountain, Arnold Peak — from Emmet Smith's cattle) within the Pasay the Horseshoe Basin country. Farther west, ten Wilderness Area. We looked east to the hazy-dreamy on the horizon, rise summits of wide-open ridges of Chopaka Mountain and the Chelan Crest and Washington Pass. were intrigued. To get there, drive the Okanogan Valley to On our way to Horseshoe Basin we met Wil Tonasket and turn west to Loomis in the Sin- lis Erwin, one of the Okanoganites chiefly lahekin Valley. -
Mt. Baker Ski Area
Winter Activity Guide Mount Baker Ranger District North Cascades National Park Contacts Get ready for winter adventure! Head east along the Mt. Baker Mt. Baker-Snoqualmie National Forest State Road Conditions: /Mt. Baker Ranger District Washington State Dept. of Transportation Highway to access National Forest 810 State Route 20 Dial 511 from within Washington State lands and the popular Mt. Baker Ski Sedro-Woolley, WA 98284 www.wsdot.wa.gov Area. Travel the picturesque North (360) 856-5700 ext. 515 Glacier Public Service Center Washington State Winter Recreation and Cascades Highway along the Skagit 10091 Mt. Baker Highway State Sno-Park Information: Wild & Scenic River System into the Glacier, WA 98244 www.parks.wa.gov/winter heart of the North Cascades. (360) 599-2714 http://www.fs.usda.gov/mbs Mt. Baker Ski Area Take some time for winter discovery but North Cascades National Park Service Ski Area Snow Report: be aware that terrain may be challenging Complex (360) 671-0211 to navigate at times. Mountain weather (360) 854-7200 www.mtbaker.us conditions can change dramatically and www.nps.gov/noca with little warning. Be prepared and check Cross-country ski & snowshoe trails along the Mt. Baker Highway: forecasts before heading out. National Weather Service www.weather.gov www.nooksacknordicskiclub.org Northwest Weather & Avalanche For eagle watching information visit: Travel Tips Center: Skagit River Bald Eagle Interpretive Center Mountain Weather Conditions www.skagiteagle.org • Prepare your vehicle for winter travel. www.nwac.us • Always carry tire chains and a shovel - practice putting tire chains on before you head out. -
Lower Stehekin River Cutthroat and Rainbow Trout Spawning Surveys, 2009
National Park Service U.S. Department of the Interior Natural Resource Program Center Lower Stehekin River cutthroat and rainbow trout spawning surveys, 2009 Natural Resource Data Series NPS/NOCA/NRDS—2010/111 ON THE COVER Surveyor stands by a Rainbow Trout Redd. Photograph by: North Cascades National Park Lower Stehekin River cutthroat and rainbow trout spawning surveys, 2009 Natural Resource Data Series NPS/NOCA/NRDS—2010/111 Hugh Anthony and Reed Glesne North Cascades National Park Service Complex 810 State Route 20 Sedro-Woolley, WA. 98284 November 2010 U.S. Department of the Interior National Park Service Natural Resource Program Center Fort Collins, Colorado The National Park Service, Natural Resource Program Center publishes a range of reports that address natural resource topics of interest and applicability to a broad audience in the National Park Service and others in natural resource management, including scientists, conservation and environmental constituencies, and the public. The Natural Resource Data Series is intended for timely release of basic data sets and data summaries. Care has been taken to assure accuracy of raw data values, but a thorough analysis and interpretation of the data has not been completed. Consequently, the initial analyses of data in this report are provisional and subject to change. All manuscripts in the series receive the appropriate level of peer review to ensure that the information is scientifically credible, technically accurate, appropriately written for the intended audience, and designed and published in a professional manner. This report received informal peer review by subject-matter experts who were not directly involved in the collection, analysis, or reporting of the data. -
108Th Congress of the United States WASHINGTON CANADA
108th Congress of the United States WASHINGTON CANADA 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 33 3 3 3 333333 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 Osoyoos Nooksack 3 3 3 3 3 3 3 Lake Trust Land 3 3 3 3 3 3 3 3 3 3 3 r 3 e 3 3 v 3 3 i 3 R 3 Birch 3 ck 3 Ross Strait of Georgia 3 sa 3 3 Bay ok 3 o 3 N 3 3 Nooksack 3 Lake 3 3 3 3 Trust Land 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 North Cascades 3 3 3 3 3 3 3 3 3 3 3 National Park 3 WHATCOM 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 PEND 3 3 3 3 3 3 3 3 3 3 3 3 3 Lummi Nooksack Res 3 3 3 3 3 3 3 3 Res 3 3 3 OREILLE 3 3 3 3 3 3 3 Bellingham 3 3 3 Bay 3 33 3 3 Pend Oreille River 3 3 3 3 3 3 3 3 3 3 3 Bellingham 3 3 3 3 3 3 3 3 3 3 3 3 3 Ross Lake 3 3 Cowlitz 3 3 3 3 3 3 3 3 3 3 3 3 3 NRA 3 3 3 3 3 3 3 3 3 3 3 3 Bay 3 3 3 3 3 3 3 Okanogan River 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 Samish 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 TDSA 3 3 3 3 3 3 3 3 3 3 3 Samish 3 3 3 3 3 3 3 3 Rosario Strait Bay 3 3 FERRY 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 Upper Skagit Res 3 SAN JUAN 3 Haro Strait 3 North Cascades 3 3 3 3 3 3 3 National Park 3 OKANOGAN Upper Skagit Res 3 3 3 3 3 3 3 3 3 Skagit River 3 3 3 3 3 3 3 Padilla 3 3 3 3 Griffin Bay 3 3 3 3 3 3 3 Bay 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 US Coast Guard Station 3 3 3 SKAGIT 3 3 3 3 3 3 3 Neah Bay 3 3 3 3 3 3 3 3 3 3 3 STEVENS 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 -
The Skagit-High Ross Controversy: Negotiation and Settlement
Volume 26 Issue 2 U.S. - Canada Transboundary Resource Issues Spring 1986 The Skagit-High Ross Controversy: Negotiation and Settlement Jackie Krolopp Kirn Marion E. Marts Recommended Citation Jackie K. Kirn & Marion E. Marts, The Skagit-High Ross Controversy: Negotiation and Settlement, 26 Nat. Resources J. 261 (1986). Available at: https://digitalrepository.unm.edu/nrj/vol26/iss2/6 This Article is brought to you for free and open access by the Law Journals at UNM Digital Repository. It has been accepted for inclusion in Natural Resources Journal by an authorized editor of UNM Digital Repository. For more information, please contact [email protected], [email protected], [email protected]. JACKIE KROLOPP KIRN* and MARION E. MARTS** The Skagit-High Ross Controversy: Negotiation and Settlement SETTING AND BACKGROUND The Skagit River is a short but powerful stream which rises in the mountains of southwestern British Columbia, cuts through the northern Cascades in a spectacular and once-remote mountain gorge, and empties into Puget Sound approximately sixty miles north of Seattle. The beautiful mountain scenery of the heavily glaciated north Cascades was formally recognized in the United States by the creation of the North Cascades National Park and the Ross Lake National Recreation Area in 1968, and earlier in British Columbia by creation of the E.C. Manning Provincial Park. The Ross Lake Recreation Area covers the narrow valley of the upper Skagit River in Washington and portions of several tributary valleys. It was created as a political and, to environmentalists who wanted national park status for the entire area, controversial, compromise which accom- modated the city of Seattle's Skagit River Project and the then-planned North Cascades Highway. -
Detailed Map Sheet; Soil Survey of North Cascades National Park
UNITED STATES DEPARTMENT OF THE INTERIOR NATIONAL PARK SERVICE SOIL SURVEY OF NORTH CASCADES NATIONAL PARK COMPLEX, WASHINGTON UNITED STATES DEPARTMENT OF AGRICULTURE MOUNT REDOUBT QUADRANGLE NATURAL RESOURCES CONSERVATION SERVICE SHEET NUMBER 3 OF 34 121°22’30"W 121°20’0"W 121°17’30"W 121°15’0"W BRITISH COLUMBIA CANADA WHATCOM COUNTY WASHINGTON UNITED STATES 49°0’0"N 49°0’0"N 9016 9008 9008 9012 8010 8009 9998 9008 9016 9003 9003 Depot 9010 Creek 9012 8011 9016 9003 9016 9008 9008 9999 9003 8006 8010 8010 Nodoubt Peak 8011 9003 9998 9016 9010 8011 8006 9008 9010 8007 8006 9010 9998 9016 9003 8010 9016 9016 9999 9016 8006 9999 9003 9016 8007 8010 9003 9010 9012 8010 9998 9998 8009 8006 9008 8009 Mt 48°57’30"N TRAIL Redoubt 48°57’30"N 8007 9016 8006 9008 REDOUBT GLACIER 9010 Bear 9003 9012 9008 9003 CHILLIWACK 8011 9003 8006 9010 8006 8000 Creek 9008 9003 Bear Mox 8007 Lake Peaks 8009 9016 9999 8007 9008 9003 9016 9010 8006 9010 9010 9998 8011 9998 9003 9003 8007 9010 9016 Spickard Mount 4, sheet Joins Joins sheet 2, Copper Mountain Copper 2, sheet Joins Bear Mountain 9010 9008 9016 9998 9010 9012 9016 8010 9010 9008 Redoubt 9016 9003 9999 9016 8009 9003 8006 9008 9010 9010 Creek 8006 9010 9008 9012 8011 48°55’0"N 48°55’0"N 9003 8010 9010 9008 8006 8007 7003 9008 8006 8011 9998 9003 9012 7015 9010 9008 9010 6009 9010 8006 9016 9003 7003 9003 9008 9016 6015 9016 9998 9003 7015 9003 9010 6010 6009 9010 9998 6015 9010 9003 9998 8007 9016 9008 9010 9012 9998 9012 9012 9003 9016 9016 9008 6015 9999 6014 9003 6009 9999Lake 9010 6009 Reveille -
Tectonic Elements and Evolution of Northwest Washington
TECTONIC ELEMENTS AND EVOLUTION OF NORTHWEST WASHINGTON by Edwin H. Brown and Joe D. Dragovich WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES Geologic Map GM-52 December 2003 DISCLAIMER This product is provided ‘as is’ without warranty of any kind, ei- ther expressed or implied, including, but not limited to, the im- plied warranties of merchantability and fitness for a particular use. The Washington Department of Natural Resources will not be liable to the user of this product for any activity involving the product with respect to the following: (a) lost profits, lost sav- ings, or any other consequential damages; (b) the fitness of the product for a particular purpose; or (c) use of the product or re- sults obtained from use of the product. This product is consid- ered to be exempt from the Geologist Licensing Act [RCW 18.220.190 (4)] because it is geological research conducted by the State of Washington, Department of Natural Resources, Di- vision of Geology and Earth Resources. WASHINGTON STATE DEPARTMENT OF NATURAL RESOURCES Doug Sutherland—Commissioner of Public Lands DIVISION OF GEOLOGY AND EARTH RESOURCES Ron Teissere—State Geologist David K. Norman—Assistant State Geologist This report is available free of charge online at http://www.dnr.wa.gov/geology/pubs/ Order a printed copy by mail from: Publications Washington Department of Natural Resources Division of Geology and Earth Resources PO Box 47007 Olympia, WA 98504-7007 E-mail: [email protected] To obtain an order form, go to: http://www.dnr.wa.gov/geology/pubs/ Published in the United States of America Tectonic Elements and Evolution of Northwest Washington Edwin H. -
The Damnation of a Dam : the High Ross Dam Controversy
THE DAMYIATION OF A DAM: TIIE HIGH ROSS DAM CONTROVERSY TERRY ALLAN SIblMONS A. B., University of California, Santa Cruz, 1968 A THESIS SUBIUTTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF ARTS in the Department of Geography SIMON FRASER UNIVERSITY May 1974 All rights reserved. This thesis may not b? reproduced in whole or in part, by photocopy or other means, without permission of the author. APPROVAL Name: Terry Allan Simmons Degree: Master of Arts Title of Thesis: The Damnation of a Dam: The High Ross Dam Controversy Examining Committee: Chairman: F. F. Cunningham 4 E.. Gibson Seni Supervisor / /( L. J. Evendon / I. K. Fox ernal Examiner Professor School of Community and Regional Planning University of British Columbia PARTIAL COPYRIGHT LICENSE I hereby grant to Simon Fraser University rhe righc to lcnd my thesis or dissertation (the title of which is shown below) to users of the Simon Fraser University Library, and to make partial or single copies only for such users or in response to a request from the library of any other university, or other educational institution, on its own behalf or for one of its users. I further agree that permission for multiple copying of this thesis for scholarly purposes may be granted by me or the Dean of Graduate Studies. It is understood that copying or publication of this thesis for financial gain shall not be allowed ' without my written permission. Title of' ~hesis /mqqmkm: The Damnation nf a nam. ~m -Author: / " (signature ) Terrv A. S.imrnonze (name ) July 22, 1974 (date) ABSTRACT In 1967, after nearly fifty years of preparation, inter- national negotiations concerning the construction of the High Ross Dan1 on the Skagit River were concluded between the Province of British Columbia and the City of Seattle. -
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