USGS Scientific Investigations Map 2940, Technical Pamphlet

Total Page:16

File Type:pdf, Size:1020Kb

USGS Scientific Investigations Map 2940, Technical Pamphlet 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 Technical 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 Geology of the North Cascade Range ........................................................................................................2 Major faults ............................................................................................................................................2 Darrington-Devils Mountain Fault Zone ...................................................................................3 Straight Creek Fault .....................................................................................................................4 Ross Lake Fault Zone ..................................................................................................................4 Pasayten Fault ..............................................................................................................................4 Geologic map units ...............................................................................................................................4 Orogenic and pre-orogenic rocks mostly west of the Straight Creek Fault ......................4 Orogenic and pre-orogenic rocks east of the Straight Creek Fault ....................................6 Rocks of late- and post-orogenic transtension ....................................................................10 Flood basalt and associated deposits ....................................................................................11 Rocks of the Cascade magmatic arc ......................................................................................11 Unconsolidated deposits ..........................................................................................................12 Description of map units .............................................................................................................................13 Unconsolidated deposits ...................................................................................................................13 Nonglacial deposits ...................................................................................................................13 Glacial deposits ..........................................................................................................................13 Glacial and nonglacial deposits ..............................................................................................14 Rocks of Cascade magmatic arc .....................................................................................................14 Flood basalt and associated deposits .............................................................................................15 Rocks of late- and post-orogenic transtension .............................................................................15 Extensional deposits .................................................................................................................15 Other rocks..................................................................................................................................16 Orogenic and pre-orogenic rocks mostly west of Straight Creek Fault ...................................16 Rocks southwest of Darrington-Devils Mountain Fault Zone ............................................16 Rocks in Darrington-Devils Mountain Fault Zone ................................................................16 Rocks northeast of Darrington-Devils Mountain Fault Zone ..............................................16 Orogenic and pre-orogenic rocks east of Straight Creek Fault ..................................................18 Rocks unique to Wenatchee block .........................................................................................18 Rocks in Wenatchee and Chelan blocks ...............................................................................18 Rocks unique to Ross Lake Fault Zone ...................................................................................20 Rocks in Methow block ............................................................................................................20 Rocks in Okanogan block .........................................................................................................21 References cited ..........................................................................................................................................22 Figures 1. Map of Northwestern Washington showing area of geologic map ............................sheet 2 2. Map showing sources of geologic data for Twisp 1:100,000 topographic quadrangle and adjacent area ............................................................................................................sheet 2 3. Sketch figure showing plate tectonic processes ...........................................................sheet 2 4. Map showing major geologic structures and major metamorphic episodes in the North Cascades, Washington ........................................................................................sheet 2 5. Generalized geologic map of North Cascades, Washinton ..........................................sheet 2 i 6. Geologic times scales relative to some geologic events in North Cascades, Washington ..................................................................................................................................3 7. Looking south from east ridge of Mount Formidable......................................................sheet 2 8. View northwest from Bacon Peak .....................................................................................sheet 2 9. Digital elevation model showing maximum extent of Cordilleran Ice Sheet in the North Cascades during the Vashon stade ...................................................................sheet 2 10. Sketch showing a north-south cross section of the Cascade Range in Washington ..................................................................................................................................2 11. Sketch of cross section showing how terranes (nappes) became stacked in the Northwest Cascades System along thrust faults during collision between tectonic plates .............................................................................................................................5 12. Granite of Cascades Pass family on the west wall of Nooksack cirque in foreground .........................................................................................................................sheet 2 13. Beds of sandstone (Eocene Swauk Formation) in older extensional deposits on south side of the east ridge of Summit Chief Mountain ............................................sheet 2 14. Disrupted sandstone, greenstone, and light-colored dikes in argillite matrix of western mélange belt unit TKwb, South Fork Stillaguamish River ..........................sheet 2 15. View east from Mount Index across Skykomish River valley to Gunn and Baring peaks, underlain by erosion-resistant tectonic slices of migmatitic gneiss in less-resistant sedimentary rocks of eastern mélange belt .....................sheet 2 16. Large lumps of erosion-resistant rock dotting serpentenite matrix of Helena- Haystack melange (units TKhm, TKhg) .........................................................................sheet 2 17. View of Eldorado Peak, looking northeast from divide between Sibley and Marble Creeks ...............................................................................................................................sheet 2 18. Sketch showing Cretaceous marine setting for accumulation of sediments that became rocks of Methow Ocean and younger deposits .....................................................9 19. View from Mount Winthrop south along Cascades Crest ...........................................sheet 2 20. Hozomeen greenstone in Methow block north of Little Beaver Creek .....................sheet 2 21. Ternary diagrams showing classification of igneous rocks by
Recommended publications
  • Strategy Habitat: Ponderosa Pine Woodlands
    Habitat: Conservation Summaries for Strategy Habitats Strategy Habitat: Ponderosa Pine Woodlands Ecoregions: Conservation Overview: Ponderosa Pine Woodlands are a Strategy Habitat in the Blue Moun- Ponderosa pine habitats historically covered a large portion of the tains, East Cascades, and Klamath Mountains ecoregions. Blue Mountains ecoregion, as well as parts of the East Cascades and Klamath Mountains. Ponderosa pine is still widely distributed in eastern Characteristics: and southern Oregon. However, the structure and species composition The structure and composition of ponderosa pine woodlands varies of woodlands have changed dramatically. Historically, ponderosa pine across the state, depending on local climate, soil type and moisture, habitats had frequent low-intensity ground fires that maintained an elevation, aspect and fire history. In Blue Mountains, East Cascades open understory. Due to past selective logging and fire suppression, and Klamath Mountains ecoregions, ponderosa pine woodlands have dense patches of smaller conifers have grown in the understory of pon- open canopies, generally covering 10-40 percent of the sky. Their derosa pine forests. Depending on the area, these conifers may include understories are variable combinations of shrubs, herbaceous plants, shade-tolerant Douglas-fir, grand fir and white fir, or young ponderosa and grasses. Ponderosa woodlands are dominated by ponderosa pine, pine and lodgepole pine. These dense stands are vulnerable to drought but may also have lodgepole, western juniper, aspen, western larch, stress, insect outbreaks, and disease. The tree layers act as ladder fuels, grand fir, Douglas-fir, incense cedar, sugar pine, or white fir, depend- increasing the chances that a ground fire will become a forest-destroy- ing on ecoregion and site conditions.
    [Show full text]
  • 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]
  • Glossary Glossary
    Glossary Glossary Albedo A measure of an object’s reflectivity. A pure white reflecting surface has an albedo of 1.0 (100%). A pitch-black, nonreflecting surface has an albedo of 0.0. The Moon is a fairly dark object with a combined albedo of 0.07 (reflecting 7% of the sunlight that falls upon it). The albedo range of the lunar maria is between 0.05 and 0.08. The brighter highlands have an albedo range from 0.09 to 0.15. Anorthosite Rocks rich in the mineral feldspar, making up much of the Moon’s bright highland regions. Aperture The diameter of a telescope’s objective lens or primary mirror. Apogee The point in the Moon’s orbit where it is furthest from the Earth. At apogee, the Moon can reach a maximum distance of 406,700 km from the Earth. Apollo The manned lunar program of the United States. Between July 1969 and December 1972, six Apollo missions landed on the Moon, allowing a total of 12 astronauts to explore its surface. Asteroid A minor planet. A large solid body of rock in orbit around the Sun. Banded crater A crater that displays dusky linear tracts on its inner walls and/or floor. 250 Basalt A dark, fine-grained volcanic rock, low in silicon, with a low viscosity. Basaltic material fills many of the Moon’s major basins, especially on the near side. Glossary Basin A very large circular impact structure (usually comprising multiple concentric rings) that usually displays some degree of flooding with lava. The largest and most conspicuous lava- flooded basins on the Moon are found on the near side, and most are filled to their outer edges with mare basalts.
    [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 Mountaineer Annual
    The Mountaineer Annual 1991-1992 The MountaineerAnnual 1991-1992 Volume 79 Published August, 1993 2 TheMountaineer Annual Beargrass on Mt. Rainier Steve Johnson The Mountaineers Purposes 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 Northwest America; To make expeditionsinto theseregions in fulfillment of the above purposes; To encourage a spirit of good fellowship among all lovers of outdoor life. Ascending Eldorado Royce Conrad 4 The Mountaineer Annual The MountaineerAnnual The continuing spirit of The Mountaineers shines through in this newest edition of The Mountaineer Annual. Thank you to all the creative people who so willingly gave their time and talent in producing this book. EditorialCommittee Judi Maxwell- Editor; Production Manager; Layout Ann Marshall -Assistant Editor Steve Johnson -Computer Editor; Mailing Fran Troje -Advertising Manager Mike Buettner- Editorial Committee George Potratz- Desktop Publishing (Communications Manager) Helen Cherullo and Marge Mueller- Production Consultants (Mountaineers Books) Virginia Felton - Executive Director Katrina Reed-Administrative Assistant Eileen Allen - Accounting Manager Steve Costie -Member Services Manager Cover Design: Judi Maxwell and Helen Cherullo Cover Photographs: Front -Ascent of Eldorado © Photo by John Roper Back- Friends in High Places © Photo by Julie Smith © 1993 by The Mountaineers All Rights Reserved Published by The Mountaineers 300Third Avenue West Seattle, Washington 98119 Printedin the United States of America Printed on recycled paper Contents The Mountaineers Purposes 3 Foreword 8 Don Heck Vision for the Twenty-First Century 11 Dianne Hoff Development of a Wilderness Ethics Policy 14 Edward M.
    [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]
  • Review Article Magma Loading in the Southern Coast Plutonic Complex, British Columbia and Washington
    GeoScienceWorld Lithosphere Volume 2020, Article ID 8856566, 17 pages https://doi.org/10.2113/2020/8856566 Review Article Magma Loading in the Southern Coast Plutonic Complex, British Columbia and Washington E. H. Brown Department of Geology, Western Washington University, USA Correspondence should be addressed to E. H. Brown; [email protected] Received 2 May 2020; Accepted 22 September 2020; Published 10 November 2020 Academic Editor: Tamer S. Abu-Alam Copyright © 2020 E. H. Brown. Exclusive Licensee GeoScienceWorld. Distributed under a Creative Commons Attribution License (CC BY 4.0). The southen end of the 1800 km long Coast Plutonic Complex (CPC), exposed in the Harrison Lake area of British Columbia and in the North Cascades of Washington, bears a record of great crustal thickening -20 to 40 km in localized zones during Late Cretaceous times. During this period, the CPC was positioned at the continental margin during collision/subduction of the Farallon plate. Arc magmatism and regional orogenic contraction were both active as potential crustal thickening processes. Magmatism is favored in this report as the dominant factor based on the delineation of four spatially and temporally separate loading events, the close association of the loaded areas with emplacement of large plutons, and a paucity of evidence of deep regional tectonic contraction. The timing and spatial location of crustal loading events are documented by the following: zircon ages in plutons; an early event of low pressure in pluton aureoles evidenced by andalusite, now pseudomorphed by high- pressure minerals; high pressures in country rock in pluton aureoles measured by mineral compositions in the assemblages garnet-biotite-muscovite-plagioclase and garnet-aluminum silicate-plagioclase; high pressures recorded in plutons by Al-in- hornblende barometry; and uplift ages of plutons derived from K-Ar and Ar-Ar ages of micas and hornblende in plutons.
    [Show full text]
  • 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.
    [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]
  • July 2020 in This Issue Online Readers, ALPO Conference November 6-7, 2020 2 Lunar Calendar July 2020 3 Click on Images an Invitation to Join ALPO 3 for Hyperlinks
    A publication of the Lunar Section of ALPO Edited by David Teske: [email protected] 2162 Enon Road, Louisville, Mississippi, USA Recent back issues: http://moon.scopesandscapes.com/tlo_back.html July 2020 In This Issue Online readers, ALPO Conference November 6-7, 2020 2 Lunar Calendar July 2020 3 click on images An Invitation to Join ALPO 3 for hyperlinks. Observations Received 4 By the Numbers 7 Submission Through the ALPO Image Achieve 4 When Submitting Observations to the ALPO Lunar Section 9 Call For Observations Focus-On 9 Focus-On Announcement 10 2020 ALPO The Walter H. Haas Observer’s Award 11 Sirsalis T, R. Hays, Jr. 12 Long Crack, R. Hill 13 Musings on Theophilus, H. Eskildsen 14 Almost Full, R. Hill 16 Northern Moon, H. Eskildsen 17 Northwest Moon and Horrebow, H. Eskildsen 18 A Bit of Thebit, R. Hill 19 Euclides D in the Landscape of the Mare Cognitum (and Two Kipukas?), A. Anunziato 20 On the South Shore, R. Hill 22 Focus On: The Lunar 100, Features 11-20, J. Hubbell 23 Recent Topographic Studies 43 Lunar Geologic Change Detection Program T. Cook 120 Key to Images in this Issue 134 These are the modern Golden Days of lunar studies in a way, with so many new resources available to lu- nar observers. Recently, we have mentioned Robert Garfinkle’s opus Luna Cognita and the new lunar map by the USGS. This month brings us the updated, 7th edition of the Virtual Moon Atlas. These are all wonderful resources for your lunar studies.
    [Show full text]
  • GEOLOGIC MAP of the CHELAN 30-MINUTE by 60-MINUTE QUADRANGLE, WASHINGTON by R
    DEPARTMENT OF THE INTERIOR TO ACCOMPANY MAP I-1661 U.S. GEOLOGICAL SURVEY GEOLOGIC MAP OF THE CHELAN 30-MINUTE BY 60-MINUTE QUADRANGLE, WASHINGTON By R. W. Tabor, V. A. Frizzell, Jr., J. T. Whetten, R. B. Waitt, D. A. Swanson, G. R. Byerly, D. B. Booth, M. J. Hetherington, and R. E. Zartman INTRODUCTION Bedrock of the Chelan 1:100,000 quadrangle displays a long and varied geologic history (fig. 1). Pioneer geologic work in the quadrangle began with Bailey Willis (1887, 1903) and I. C. Russell (1893, 1900). A. C. Waters (1930, 1932, 1938) made the first definitive geologic studies in the area (fig. 2). He mapped and described the metamorphic rocks and the lavas of the Columbia River Basalt Group in the vicinity of Chelan as well as the arkoses within the Chiwaukum graben (fig. 1). B. M. Page (1939a, b) detailed much of the structure and petrology of the metamorphic and igneous rocks in the Chiwaukum Mountains, further described the arkoses, and, for the first time, defined the alpine glacial stages in the area. C. L. Willis (1950, 1953) was the first to recognize the Chiwaukum graben, one of the more significant structural features of the region. The pre-Tertiary schists and gneisses are continuous with rocks to the north included in the Skagit Metamorphic Suite of Misch (1966, p. 102-103). Peter Misch and his students established a framework of North Cascade metamorphic geology which underlies much of our construct, especially in the western part of the quadrangle. Our work began in 1975 and was essentially completed in 1980.
    [Show full text]
  • 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.
    [Show full text]