DOCSLIB.ORG

Climate Change Vulnerability and Adaptation in the North Cascades Region, Washington

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Climate Change Vulnerability and Adaptation in the North Cascades Region, Washington United States Department of Agriculture Climate Change Vulnerability and Adaptation in the North Cascades Region, Washington Forest Pacific Northwest General Technical Report September Service Research Station PNW-GTR-892 2014 Non-Discrimination Policy The U.S. Department of Agriculture (USDA) prohibits discrimination against its customers, employees, and applicants for employment on the bases of race, color, national origin, age, disability, sex, gender identity, religion, reprisal, and where applicable, political beliefs, marital status, familial or parental status, sexual orientation, or all or part of an individual’s income is derived from any public assistance program, or protected genetic information in employ- ment or in any program or activity conducted or funded by the Department. (Not all prohibited bases will apply to all programs and/or employment activities.) To File an Employment Complaint If you wish to file an employment complaint, you must contact your agency’s EEO Counselor (PDF) within 45 days of the date of the alleged discriminatory act, event, or in the case of a personnel action. Additional information can be found online at http://www.ascr.usda.gov/ complaint_filing_file.html. To File a Program Complaint If you wish to file a Civil Rights program complaint of discrimination, complete the USDA Program Discrimination Complaint Form (PDF), found online at http://www.ascr.usda.gov/ complaint_filing_cust.html, or at any USDA office, or call (866) 632-9992 to request the form. You may also write a letter containing all of the information requested in the form. Send your completed complaint form or letter to us by mail at U.S. Department of Agriculture, Director, Office of Adjudication, 1400 Independence Avenue, S.W., Washington, D.C. 20250-9410, by fax (202) 690-7442 or email at [email protected]. Persons with Disabilities Individuals who are deaf, hard of hearing or have speech disabilities and you wish to file either an EEO or program complaint please contact USDA through the Federal Relay Service at (800) 877-8339 or (800) 845-6136 (in Spanish). Persons with disabilities, who wish to file a program complaint, please see information above on how to contact us by mail directly or by email. If you require alternative means of com- munication for program information (e.g., Braille, large print, audiotape, etc.) please contact USDA’s TARGET Center at (202) 720-2600 (voice and TDD). Supplemental Nutrition Assistance Program For any other information dealing with Supplemental Nutrition Assistance Program (SNAP) issues, persons should either contact the USDA SNAP Hotline Number at (800) 221-5689, which is also in Spanish or call the State Information/Hotline Numbers. All Other Inquiries For any other information not pertaining to civil rights, please refer to the listing of the USDA Agencies and Offices for specific agency information. Editors Crystal L. Raymond is a climate change strategic advisor, City of Seattle, Seattle City Light, 700 5th Avenue, Seattle, WA 98124 (formerly, research biologist, U.S. Department of Agriculture, Forest Service, Pacific Northwest Research Station, Pacific Wildland Fire Sciences Laboratory, Seattle, WA); David L. Peterson is a research biological scientist, U.S. Department of Agriculture, Forest Service, Pacific Northwest Research Station, Pacific Wildland Fire Sciences Laboratory, 400 N 34th Street, Suite 201, Seattle, WA 98103; and Regina M. Rochefort is a science advisor, U.S. Department of the Interior, National Park Service, North Cascades National Park Complex, 2105 State Route 20, Sedro-Woolley, WA 98284. Cover photo by Victor Mesny Climate Change Vulnerability and Adaptation in the North Cascades Region, Washington Crystal L. Raymond, David L. Peterson, and Regina M. Rochefort Editors U.S. Department of Agriculture, Forest Service Pacific Northwest Research Station Portland, Oregon General Technical Report, PNW-GTR-892 September 2014 Abstract Raymond, Crystal L.; Peterson, David L.; Rochefort, Regina M., eds. 2014. Climate change vulnerability and adaptation in the North Cascades region, Washington. Gen. Tech. Rep. PNW-GTR-892. Portland, OR: U.S. Department of Agriculture, Forest Service, Pacific Northwest Research Station. 279 p. The North Cascadia Adaptation Partnership (NCAP) is a science-management partnership consisting of the U.S. Department of Agriculture Forest Service Mount Baker-Snoqualmie and Okanogan-Wenatchee National Forests and Pacific North- west Research Station; North Cascades National Park Complex; Mount Rainier National Park; and University of Washington Climate Impacts Group. These organizations worked with numerous stakeholders over 2 years to identify climate change issues relevant to resource management in the North Cascades and to find solutions that will facilitate the transition of the diverse ecosystems of this region into a warmer climate. The NCAP provided education, conducted a climate change vulnerability assessment, and developed adaptation options for federal agencies that manage 2.4 million hectares in north-central Washington. In the Pacific Northwest, the current warming trend is expected to continue, with average warming of 2.1 °C by the 2040s and 3.8 °C by the 2080s; precipitation may vary slightly, but the magnitude and direction are uncertain. This warming will have far-reaching effects on aquatic and terrestrial ecosystems. Hydrologic sys- tems will be especially vulnerable as North Cascades watersheds become increas- ingly rain dominated, rather than snow dominated, resulting in more autumn/winter flooding, higher peak flows, and lower summer flows. This will greatly affect the extensive road network in the North Cascades (longer than 16 000 km), making it difficult to maintain access for recreational users and resource managers. It will also greatly reduce suitable fish habitat, especially as stream temperatures increase above critical thresholds. In forest ecosystems, higher temperatures will increase stress and lower the growth and productivity of lower elevation tree species on both the western and eastern sides of the Cascade crest, although growth of high- elevation tree species is expected to increase. Distribution and abundance of plant species may change over the long term, and increased disturbance (wildfire, insects, and invasive species) will cause rapid changes in ecosystem structure and function across broad landscapes, especially on the east side. This in turn will alter habitat for a wide range of animal species by potentially reducing connectivity and late- successional forest structure. Coping with and adapting to the effects of an altered climate will become increasingly difficult after the mid-21st century, although adaptation strategies and tactics are available to ease the transition to a warmer climate. For roads and infrastructure, tactics for increasing resistance and resilience to higher peak flows include installing hardened stream crossings, stabilizing streambanks, design- ing culverts for projected peak flows, and upgrading bridges and increasing their height. For fisheries, tactics for increasing resilience of salmon to altered hydrology and higher stream temperature include restoring stream and floodplain complex- ity, reducing road density near streams, increasing forest cover to retain snow and decrease snow melt, and identifying and protecting cold-water refugia. For vegetation, tactics for increasing resilience to higher temperature and increased disturbance include accelerating development of late-successional forest conditions by reducing density and diversifying forest structure, managing for future range of variability in structure and species, including invasive species prevention strategies in all projects, and monitoring changes in tree distribution and establishment at tree line. For wildlife, tactics for increasing resilience to altered habitat include increas- ing diversity of age classes and restoring a patch mosaic, increasing fuel reduction treatments in dry forests, using conservation easements to maintain habitat connec- tivity, and removing exotic fish species to protect amphibian populations. The NCAP facilitated the largest climate change adaptation effort on federal lands to date by including many participants from other organizations to promote an all-lands approach to addressing climate change. It achieved specific elements of national climate change strategies for the U.S. Forest Service and National Park Service, providing a scientific foundation for resource management and planning in the North Cascades region. Rapid implementation of adaptation in sustainable resource management will enhance the potential for North Cascades ecosystems to maintain long-term functionality in future decades. Keywords: Access, adaptation, climate change, fire, forest ecosystems, fisher- ies, hydrology, North Cascade Range, North Cascadia Adaptation Partnership, roads, science-management partnership, vegetation, wildlife. Contents 1 Chapter 1: Introduction Crystal L. Raymond, David L. Peterson, and Regina M. Rochefort 1 Climate Change Responses of the Forest Service and National Park Service 3 Science-Management Partnerships 5 The North Cascadia Adaptation Partnership Process 8 All-Lands Approach to Climate Change Adaptation 10 Literature Cited 15 Chapter 2: Ecological, Biogeographical, and Historical Context of the North Cascade Range Kailey Marcinkowski, Crystal L. Raymond, and Lee K. Cerveny 16 Ecological Setting 17 Cultural History of the North Cascades 18 Geography, History,
Load more

Recommended publications
  • 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
    [Show full text]
  • 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).
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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).
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]