Climate Change Vulnerability and Adaptation in the North Cascades Region, Washington
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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 Complete Script
Feb rua rg 1968 North Cascades Conservation Council P. 0. Box 156 Un ? ve rs i ty Stat i on Seattle, './n. 98 105 SCRIPT FOR NORTH CASCAOES SLIDE SHOW (75 SI Ides) I ntroduct Ion : The North Cascades fiountatn Range In the State of VJashington Is a great tangled chain of knotted peaks and spires, glaciers and rivers, lakes, forests, and meadov;s, stretching for a 150 miles - roughly from Pt. fiainier National Park north to the Canadian Border, The h undreds of sharp spiring mountain peaks, many of them still unnamed and relatively unexplored, rise from near sea level elevations to seven to ten thousand feet. On the flanks of the mountains are 519 glaciers, in 9 3 square mites of ice - three times as much living ice as in all the rest of the forty-eight states put together. The great river valleys contain the last remnants of the magnificent Pacific Northwest Rain Forest of immense Douglas Fir, cedar, and hemlock. f'oss and ferns carpet the forest floor, and wild• life abounds. The great rivers and thousands of streams and lakes run clear and pure still; the nine thousand foot deep trencli contain• ing 55 mile long Lake Chelan is one of tiie deepest canyons in the world, from lake bottom to mountain top, in 1937 Park Service Study Report declared that the North Cascades, if created into a National Park, would "outrank in scenic quality any existing National Park in the United States and any possibility for such a park." The seven iiiitlion acre area of the North Cascades is almost entirely Fedo rally owned, and managed by the United States Forest Service, an agency of the Department of Agriculture, The Forest Ser• vice operates under the policy of "multiple use", which permits log• ging, mining, grazing, hunting, wt Iderness, and alI forms of recrea• tional use, Hov/e ve r , the 1937 Park Study Report rec ornmen d ed the creation of a three million acre Ice Peaks National Park ombracing all of the great volcanos of the North Cascades and most of the rest of the superlative scenery. -
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. -
Geologic History of Siletzia, a Large Igneous Province in the Oregon And
Geologic history of Siletzia, a large igneous province in the Oregon and Washington Coast Range: Correlation to the geomagnetic polarity time scale and implications for a long-lived Yellowstone hotspot Wells, R., Bukry, D., Friedman, R., Pyle, D., Duncan, R., Haeussler, P., & Wooden, J. (2014). Geologic history of Siletzia, a large igneous province in the Oregon and Washington Coast Range: Correlation to the geomagnetic polarity time scale and implications for a long-lived Yellowstone hotspot. Geosphere, 10 (4), 692-719. doi:10.1130/GES01018.1 10.1130/GES01018.1 Geological Society of America Version of Record http://cdss.library.oregonstate.edu/sa-termsofuse Downloaded from geosphere.gsapubs.org on September 10, 2014 Geologic history of Siletzia, a large igneous province in the Oregon and Washington Coast Range: Correlation to the geomagnetic polarity time scale and implications for a long-lived Yellowstone hotspot Ray Wells1, David Bukry1, Richard Friedman2, Doug Pyle3, Robert Duncan4, Peter Haeussler5, and Joe Wooden6 1U.S. Geological Survey, 345 Middlefi eld Road, Menlo Park, California 94025-3561, USA 2Pacifi c Centre for Isotopic and Geochemical Research, Department of Earth, Ocean and Atmospheric Sciences, 6339 Stores Road, University of British Columbia, Vancouver, BC V6T 1Z4, Canada 3Department of Geology and Geophysics, University of Hawaii at Manoa, 1680 East West Road, Honolulu, Hawaii 96822, USA 4College of Earth, Ocean, and Atmospheric Sciences, Oregon State University, 104 CEOAS Administration Building, Corvallis, Oregon 97331-5503, USA 5U.S. Geological Survey, 4210 University Drive, Anchorage, Alaska 99508-4626, USA 6School of Earth Sciences, Stanford University, 397 Panama Mall Mitchell Building 101, Stanford, California 94305-2210, USA ABSTRACT frames, the Yellowstone hotspot (YHS) is on southern Vancouver Island (Canada) to Rose- or near an inferred northeast-striking Kula- burg, Oregon (Fig. -
Information Circular 41: Origin of Cascade Landscapes
111ackin I CdrlJ .rc-1J ORIGIN OF CASCADE LANDSCAPES ---=-~--=---------=---- FRONTISPIECE Picket Range in upper Skagit area, Northern Cascade Mountains. Snowfields occupy a former ice-filled cirque. Grass is enroaching on ice-polished rock surfaces. State of Washington DANIEL J. EVANS, Governor Department of Conservation ROY MUNDY, Director DIVISION OF MINES AND GEOLOGY MARSHALL T. HUNTTING, SupervisoT Information Circular No. 41 ORIGIN OF CASCADE LANDSCAPES By J. HOOVER MACKIN and ALLENS. CARY STATE PRINTING PLANT, OLYMPIA, WASHINGTON 1965 For sale by Department of Conservation, Olympia, Washington. Price, 50 cents. FOREWORD The Cascade Range has had an important influence on the lives of a great many people ever since man has inhabited the Northwest. The mountains were a barrier to Indian travel; they were a challenge to the westward migration of the early settlers in the area; they posed serious problems for the early railroad builders; and they still constitute an obstruction to east-west travel. A large part of the timber, mineral, and surface water resources of the State come from the Cascades. About 80 percent of the area covered by glaciers in the United States, exclusive of Alaska, is in the Cascades of Washington. This region includes some of the finest mountain scenery in the country and is a popular outdoor recreation area. The Cascade Range is a source of economic value to many, a source of pleasure to many others, and a problem or source of irritation to some. Regardless of their reactions, many people have wondered about the origin of the mountains How and when did the Cascades come into being, and what forces were responsible for the construction job? -This report, "Origin of Cascade Landscapes," gives the answers to these questions. -
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. -
Chapter 15 Comparative Phylogeography of North- Western North America: a Synthesis
Chapter 15 Comparative phylogeography of north- western North America: a synthesis S. J. Brunsfeld,* J. Sullivan,†D. E. Soltis‡and P. S. Soltis§ Introduction Phylogeography is concerned with the principles and processes that determine the geographic distributions of genealogical lineages, within and among closely related species (Avise et al. 1987;Avise 2000).Although this field of study is very new (only a little more than a decade has passed since the term ‘phylogeography’was first coined; see Avise et al. 1987),the scientific literature in this research area is now voluminous. To date, most phylogeographic investigations of natural populations have focused on muticellular animals (Hewitt 1993; Patton et al. 1994; daSilva & Patton 1998; Eizirik et al. 1998;Avise 2000; Hewitt 2000; Schaal & Olsen 2000; Sullivan et al. 2000). This bias is due in large part to the ready availability of population-level genetic markers afforded by the animal mitochondrial genome. The more slowly evolving chloroplast genome,in contrast,often does not provide sufficient variation to reconstruct phylogeny at the populational level (Soltis et al. 1997; Schaal et al. 1998; Schaal & Olsen 2000). Phylogeographic data have accumulated so rapidly for animal taxa that it has been possible to compare phylogeographic structure among codistributed species. In fact, one of the most profound recent contributions of molecular phylogeography is the construction of regional phylogeographic perspec- tives that permit comparisons of phylogeographic structure among codistributed species, and subsequent integration of genealogical data with independent biogeo- graphic and systematic data. Probably the best-known regional phylogeographic analysis for North America involves animals from the southeastern USA (reviewed in Avise 2000). -
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. -
1967, Al and Frances Randall and Ramona Hammerly
The Mountaineer I L � I The Mountaineer 1968 Cover photo: Mt. Baker from Table Mt. Bob and Ira Spring Entered as second-class matter, April 8, 1922, at Post Office, Seattle, Wash., under the Act of March 3, 1879. Published monthly and semi-monthly during March and April by The Mountaineers, P.O. Box 122, Seattle, Washington, 98111. Clubroom is at 719Y2 Pike Street, Seattle. Subscription price monthly Bulletin and Annual, $5.00 per year. The Mountaineers To explore and study the mountains, forests, and watercourses of the Northwest; To gather into permanent form the history and traditions of this region; To preserve by the encouragement of protective legislation or otherwise the natural beauty of North west America; To make expeditions into these regions m fulfill ment of the above purposes; To encourage a spirit of good fellowship among all lovers of outdoor life. EDITORIAL STAFF Betty Manning, Editor, Geraldine Chybinski, Margaret Fickeisen, Kay Oelhizer, Alice Thorn Material and photographs should be submitted to The Mountaineers, P.O. Box 122, Seattle, Washington 98111, before November 1, 1968, for consideration. Photographs must be 5x7 glossy prints, bearing caption and photographer's name on back. The Mountaineer Climbing Code A climbing party of three is the minimum, unless adequate support is available who have knowledge that the climb is in progress. On crevassed glaciers, two rope teams are recommended. Carry at all times the clothing, food and equipment necessary. Rope up on all exposed places and for all glacier travel. Keep the party together, and obey the leader or majority rule. Never climb beyond your ability and knowledge. -
GEOLOGIC MAP of the MOUNT ADAMS VOLCANIC FIELD, CASCADE RANGE of SOUTHERN WASHINGTON by Wes Hildreth and Judy Fierstein
U.S. DEPARTMENT OF THE INTERIOR TO ACCOMPANY MAP 1-2460 U.S. GEOLOGICAL SURVEY GEOLOGIC MAP OF THE MOUNT ADAMS VOLCANIC FIELD, CASCADE RANGE OF SOUTHERN WASHINGTON By Wes Hildreth and Judy Fierstein When I climbed Mount Adams {17-18 August 1945] about 1950 m (6400') most of the landscape is mantled I think I found the answer to the question of why men by dense forests and huckleberry thickets. Ten radial stake everything to reach these peaks, yet obtain no glaciers and the summit icecap today cover only about visible reward for their exhaustion... Man's greatest 2.5 percent (16 km2) of the cone, but in latest Pleis experience-the one that brings supreme exultation tocene time (25-11 ka) as much as 80 percent of Mount is spiritual, not physical. It is the catching of some Adams was under ice. The volcano is drained radially vision of the universe and translating it into a poem by numerous tributaries of the Klickitat, White Salmon, or work of art ... Lewis, and Cis pus Rivers (figs. 1, 2), all of which ulti William 0. Douglas mately flow into the Columbia. Most of Mount Adams and a vast area west of it are Of Men and Mountains administered by the U.S. Forest Service, which has long had the dual charge of protecting the Wilderness Area and of providing a network of logging roads almost INTRODUCTION everywhere else. The northeast quadrant of the moun One of the dominating peaks of the Pacific North tain, however, lies within a part of the Yakima Indian west, Mount Adams, stands astride the Cascade crest, Reservation that is open solely to enrolled members of towering 3 km above the surrounding valleys.