Stratigraphy, Age, and Provenance of the Eocene Chumstick Basin
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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. -
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. -
Petrographic Data for Plutonic Rocks and Gneisses of the Glacier Peak Wilderness and Vicinity, Northern Cascades, Washington By
DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY Petrographic data for plutonic rocks and gneisses of the Glacier Peak Wilderness and vicinity, northern Cascades, Washington by Arthur B. Ford , James L. Drinkwater , and Steven L. Garwin* Open File Report 85-432 This report is preliminary and has not been reviewed for conformity with U.S, Geological Survey editorial standards and strati graphic nomenclature. ^Menlo Park, California 1988 CONTENTS Page Introduction 1 Acknowledgements 5 Methods 5 Data summaries 9 Data reports (table no. in parenthesis) Mount Bucklndy pluton (l) 29 Cascade Pass pluton (2) 32 Cloudy Pass batholith (3) 35 South Cascade Glacier stock (4) 39 Railroad Creek pluton (5) 42 Duncan Hill pluton (6) 46 Clark Mountain stocks (7) 49 High Pass pluton (8) 51 Cyclone Lake pluton (9) 54 Downey Creek pluton (10) 57 Tonalite of Bench Lake (11) 60 Sulphur Mountain pluton (12) 63 Jordan Lakes pluton (13) 66 Sloan Creek plutons (14) 69 Tenpeak pluton (15) 72 Seven-fingered Jack and Entiat plutons (16) 77 .Hoiden Lake pluton (17) 80 Cardinal Peak pluton (18) 83 Mount ChavaT pluton (19) 86 Riddle Peaks pluton (20) 90 Marblemount Meta Quartz Diorite (21) 94 Dumbell Mountain plutons (22) 97 Magic Mountain Gneiss (23) 100 Leroy Creek pluton (24) 103 Eldorado Orthogneiss (25) 106 Skagit Gneiss (26) 109 Swakane Biotite Gneiss (27) 112 Miscellaneous small plutons (28) 116 Sitkum stock 117 White Chuck Glacier stock 117 Cool stock 117 Dead Duck pluton 117 Foam Creek stock 117 Downey Mountain stock 117 Grassy Point stock 118 Hidden Lake stock 118 Pear Lake pluton 118 References 119 ILLUSTRATIONS Figure Page 1. -
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. -
Accomplishments During 1976
The United States Geological Survey in Alaska: Accomplishments During 1976 Kathleen M. Blean, Editor GEOLOGICAL SURVEY CIRCULAR 751-B 1977 United States Department of the Interior CECIL D. ANDRUS, Secretary Geological Survey V. E. McKelvey, Director Free on application to Branch of Distribution, U.S. Geological Survey, 1200 South Eads Street, Arlington, VA 22202 CONTENTS Page Page Abstract ....................................................................................... Bl Northern Alaska Summary of important results, 1976 .....................................1 Continued Introduction .............................................................................1 Carboniferous microfacies, microfossils, and Statewide projects ................................................................. 1 corals, Lisburne Group, arctic Alaska, by Preliminary geologic map of Alaska, by Augustus K. Armstrong and Helen M. Beikman ................................................... 1 Bernard L. Mamet ............................................... B18 Mineral resources of Alaska, by Mississippian microfacies of the Lisburne Edward H. Cobb ....................................................... 1 Group, Endicott Mountains, arctic Alaska, A new radiometric date for the Ordovician- by August K. Armstrong and Silurian boundary, by M. A. Lanphere, Bernard L. Mamet ............................................... ...18 Michael Churkin, Jr., and G. D. Eberlein ....... 4 Late Paleozoic carbonates from the south- A new Ordovician time scale based on central -
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. -
Midcretaceous Thrusting in the Southern Coast Belt, British
TECTONICS, VOL. 15, NO. 2, PAGES, 545-565, JUNE 1996 Mid-Cretaceous thrusting in the southern Coast Belt, British Columbia and Washington, after strike-slip fault reconstruction Paul J. Umhoefer Departmentof Geology,Northern Arizona University, Flagstaff Robert B. Miller Departmentof Geology, San JoseState University, San Jose,California Abstract. A major thrust systemof mid-Cretaceousage Introduction is presentalong much of the Coast Belt of northwestern. The Coast Belt in the northwestern Cordillera of North North America. Thrusting was concurrent,and spatially America containsthe roots of the largest Mesozoic mag- coincided,with emplacementof a great volume of arc intrusives and minor local strike-slip faulting. In the maticarc in North America, which is cut by a mid-Creta- southernCoast Belt (52ø to 47øN), thrusting was followed ceous,synmagmatic thrust system over muchof its length by major dextral-slipfaulting, which resultedin significant (Figure 1) [Rubin et al., 1990]. This thrust systemis translationalshuffling of the thrust system. In this paper, especiallywell definedin SE Alaska [Brew et al., 1989; Rubin et al., 1990; Gehrels et al., 1992; Haeussler, 1992; we restorethe displacementson major dextral-slipfaults of the southernCoast Belt and then analyze the mid-Creta- McClelland et al., 1992; Rubin and Saleeby,1992] and the southern Coast Belt of SW British Columbia and NW ceousthrust system. Two reconstructionswere madethat usedextral faulting on the Yalakom fault (115 km), Castle Washington(Figure 1)[Crickmay, 1930; Misch, 1966; Davis et al., 1978; Brown, 1987; Rusrnore aad Pass and Ross Lake faults (10 km), and Fraser fault (100 Woodsworth, 199 la, 1994; Miller and Paterson, 1992; km). The reconstructionsdiffer in the amount of dextral offset on the Straight Creek fault (160 and 100 km) and Journeayand Friedman, 1993; Schiarizza et al. -
Preliminary Geologic Map of the Mount Baker 30- by 60-Minute Quadrangle, Washington
U.S. DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY Preliminary Geologic Map of the Mount Baker 30- by 60-Minute Quadrangle, Washington by R.W. Tabor1 , R.A. Haugerud2, D.B. Booth3, and E.H. Brown4 Prepared in cooperation with the Washington State Department of Natural Resources, Division of Geology and Earth Resources, Olympia, Washington, 98504 OPEN FILE REPORT 94-403 This report is preliminary and has not been reviewed for conformity with U.S.Geological Survey editorial standards or with the North American Stratigraphic Code. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government. iu.S.G.S., Menlo Park, California 94025 2U.S.G.S., University of Washington, AJ-20, Seattle, Washington 98195 3SWMD, King County Department of Public Works, Seattle, Washington, 98104 ^Department of Geology, Western Washington University, Bellingham, Washington 98225 INTRODUCTION The Mount Baker 30- by 60-minute quadrangle encompasses rocks and structures that represent the essence of North Cascade geology. The quadrangle is mostly rugged and remote and includes much of the North Cascade National Park and several dedicated Wilderness areas managed by the U.S. Forest Service. Geologic exploration has been slow and difficult. In 1858 George Gibbs (1874) ascended the Skagit River part way to begin the geographic and geologic exploration of the North Cascades. In 1901, Reginald Daly (1912) surveyed the 49th parallel along the Canadian side of the border, and George Smith and Frank Calkins (1904) surveyed the United States' side. Daly's exhaustive report was the first attempt to synthesize what has become an extremely complicated geologic story. -
Geologic Map of the North Cascade Range, Washington by Ralph A
Prepared in cooperation with Washington State Division of Geology and Earth Resources, U.S. National Park Service, and U.S. Forest Service Geologic Map of the North Cascade Range, Washington By Ralph A. Haugerud and Rowland W. Tabor Nontechnical pamphlet to accompany Scientific Investigations Map 2940 Looking south from the North Klawatti Glacier [Mbse]. In the right foreground, the glacier breaks into a heavily crevassed icefall where it descends steeply. Rock in the foreground knob is Eldorado Orthogneiss (unit TKgo), a 90 million-year-old stitching pluton, which here includes numerous dikes of light- colored pegmatite. Mount Buckner on the left skyline and Mount Forbidden hidden in clouds are also eroded from the Eldorado Orthogneiss (photographed in 1987). 2009 U.S. Department of the Interior U.S. Geological Survey CONTENTS Introduction.....................................................................................................................................................1 Using this report ....................................................................................................................................1 Map preparation ...................................................................................................................................1 Major sources of new data .................................................................................................................1 Acknowledgments ................................................................................................................................2 -
1968 Mountaineer Outings
The Mountaineer The Mountaineer 1969 Cover Photo: Mount Shuksan, near north boundary North Cascades National Park-Lee Mann 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 June by The Mountaineers, P.O. Box 122, Seattle, Washington 98111. Clubroom is at 7191h Pike Street, Seattle. Subscription price monthly Bulletin and Annual, $5.00 per year. EDITORIAL STAFF: Alice Thorn, editor; Loretta Slat er, Betty Manning. Material and photographs should be submitted to The Mountaineers, at above address, before Novem ber 1, 1969, for consideration. Photographs should be black and white glossy prints, 5x7, with caption and photographer's name on back. Manuscripts should be typed double-spaced and include writer's name, address and phone number. foreword Since the North Cascades National Park was indubi tably the event of this past year, this issue of The Mountaineer attempts to record aspects of that event. Many other magazines and groups have celebrated by now, of course, but hopefully we have managed to avoid total redundancy. Probably there will be few outward signs of the new management in the park this summer. A great deal of thinking and planning is in progress as the Park Serv ice shapes its policies and plans developments. The North Cross-State highway, while accessible by four wheel vehicle, is by no means fully open to the public yet. So, visitors and hikers are unlikely to "see" the changeover to park status right away. But the first articles in this annual reveal both the thinking and work which led to the park, and the think ing which must now be done about how the park is to be used. -
Fabric Study and Structural History of Deformed Plutonic and Metamorphic Rocks in the Holden Area, North Cascades, Washington
Western Washington University Western CEDAR WWU Graduate School Collection WWU Graduate and Undergraduate Scholarship Spring 1991 Fabric Study and Structural History of Deformed Plutonic and Metamorphic Rocks in the Holden Area, North Cascades, Washington Gary K. Hurban Western Washington University Follow this and additional works at: https://cedar.wwu.edu/wwuet Part of the Geology Commons Recommended Citation Hurban, Gary K., "Fabric Study and Structural History of Deformed Plutonic and Metamorphic Rocks in the Holden Area, North Cascades, Washington" (1991). WWU Graduate School Collection. 924. https://cedar.wwu.edu/wwuet/924 This Masters Thesis is brought to you for free and open access by the WWU Graduate and Undergraduate Scholarship at Western CEDAR. It has been accepted for inclusion in WWU Graduate School Collection by an authorized administrator of Western CEDAR. For more information, please contact [email protected]. FABRIC STUDY AND STRUCTURAL HISTORY OF DEFORMED PLUTONIC AND METAMORPHIC ROCKS IN THE HOLDEN AREA, NORTH CASCADES, WASHINGTON by Gary K. Hurban Accepted in Partial Completion of the Requirements for the Degree Master of Science Dean of Graduate School Advisory Committee 7 Chair MASTER'S THESIS In presenting this thesis in partial fulfillment of the requirements for a master's degree at Western Washington University, I agree that the Library shall make its copies freely available for inspection. I further agree that extensive copying of this thesis is allowable only for scholarly purposes. It is understood, however, that any copying or publication of this thesis for commercial purposes, or for financial gain, shall not be allowed without my written permission. Signature FABRIC STUDY AND STRUCTURAL HISTORY OF DEFORMED PLUTONIC AND METAMORPHIC ROCKS IN THE HOLDEN AREA, NORTH CASCADES, WASHING TON A thesis Presented to The Faculty of Western Washington University In Partial Fulfillment of the Requirements for the Degree Master of Science by Gary K. -
By David A. Brew'' and Arthur B. Ford1 This Report Is Preliminary and Has
U. S. DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY THE COAST MOUNTAINS PLUTONIC-METAMORPHIC COMPLEX AND RELATED ROCKS BETWEEN HAINES, ALASKA, AND FRASER, BRITISH COLUMBIA- TECTONIC AND GEOLOGIC SKETCHES AND KLONDIKE HIGHWAY ROAD LOG By David A. Brew'' and Arthur B. Ford 1 OPEN-FILE REPORT 94-268 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards or with the North American Stratigraphic Code. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government 1 U.S. Geological Survey, MS 904 Menlo Park, CA 94025 1994 THE COAST MOUNTAINS PLUTONIC-METAMORPHIC COMPLEX AND RELATED ROCKS BETWEEN HAINES, ALASKA, AND FRASER, BRITISH COLUMBIA- TECTONIC AND GEOLOGIC SKETCHES AND KLONDIKE HIGHWAY ROAD LOG David A. Brew and Arthur B. Ford U.S. Geological Survey, Branch of Alaskan Geology MS 904, 345 Middlefield Road, Menlo Park, CA 94025-3591 INTRODUCTION This guide is intended to cover four main topics pertaining to the region that includes the Skagway, Alaska, to Fraser, British Columbia, Klondike highway: (1) general tectonic setting; (2) general characteristics of the Coast Mountains plutonic-metamorphic complex (CMPMC); (3) road log with a description of the geology traversed and more specific information for selected stops; and (4) references for those interested in pursuing the details further. The guide covers not only the Klondike Highway, but also the area from Skagway south to Haines, Alaska. From here on, this whole area is referred to as the Skagway transect. Figure 1 is a lithotectonic terrane map of southeastern Alaska and an index map showing the area covered by the geologic sketch map (Fig.