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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. -
Structure and Emplacement of the Eocene Golden Horn Batholith, North Cascades, Washington
San Jose State University SJSU ScholarWorks Master's Theses Master's Theses and Graduate Research Spring 2018 Structure and Emplacement of the Eocene Golden Horn Batholith, North Cascades, Washington Christopher Scudder San Jose State University Follow this and additional works at: https://scholarworks.sjsu.edu/etd_theses Recommended Citation Scudder, Christopher, "Structure and Emplacement of the Eocene Golden Horn Batholith, North Cascades, Washington" (2018). Master's Theses. 4919. DOI: https://doi.org/10.31979/etd.p6p4-am45 https://scholarworks.sjsu.edu/etd_theses/4919 This Thesis is brought to you for free and open access by the Master's Theses and Graduate Research at SJSU ScholarWorks. It has been accepted for inclusion in Master's Theses by an authorized administrator of SJSU ScholarWorks. For more information, please contact [email protected]. STRUCTURE AND EMPLACEMENT OF THE EOCENE GOLDEN HORN BATHOLITH, NORTH CASCADES, WASHINGTON A Thesis Presented to The Faculty of the Department of Geology San José State University In Partial Fulfillment of the Requirement for the Degree Master of Science by Christopher A. Scudder May 2018 © 2018 Christopher A. Scudder ALL RIGHTS RESERVED The Designated Thesis Committee Approves the Thesis Titled STRUCTURE AND EMPLACEMENT OF THE EOCENE GOLDEN HORN BATHOLITH, NORTH CASCADES, WASHINGTON by Christopher A. Scudder APPROVED FOR THE DEPARTMENT OF GEOLOGY SAN JOSÉ STATE UNIVERSITY May 2018 Dr. Robert Miller Department of Geology Dr. Ellen Metzger Department of Geology Dr. Jonathan Miller Department of Geology ABSTRACT STRUCTURE AND EMPLACEMENT OF THE EOCENE GOLDEN HORN BATHOLITH, NORTH CASCADES, WASHINGTON By Christopher A. Scudder The 48 Ma Golden Horn batholith is a ~310 km2, shallow intrusion constructed of sub-horizontal sheets in the crystalline core of the North Cascades of Washington. -
Distribution and Abundance of Mountain Goats Within the Ross Lake Watershed, North Cascades National Park Service Complex
' I ; q£ 04. & 9) -~o3 Distribution and Abundance of Mountain Goats within the Ross Lake Watershed, North Cascades National Park Service Complex Final Report to Skagit Environmental Endowment Commission Sarah J. Welch Robert C. Kuntz II Ronald E. Holmes Roger G. Christophersen North Cascades National Park Service Complex 2105 State Route 20 Sedro-Woolley, Washington 98284-9314 December 1997 1997 SEC #10 . ' Table of Contents I. Introduction 1 2. Study Area 3. Methods 3 4. Results. 4 5. Discussion 5 6. Recommendations 6 7. Literature Cited 7 List of Figures 1. Figure 1: Mountain goat study area in Ross Lake watershed, North Cascades National Park Service Complex (1996-1997) 2 List of Tables 1. Table l: Mountain goat observations. 4 2. Table 2: Habitat characteristics where mountain goats were observed 5 Distribution and Abundance of Mountain Goats within the Ross Lake Watershed, North Cascades National Park Service Complex Introduction Mountain goats (Oreamnus americanus) are native to northwestern North America and can be found throughout the North Cascades National Park Service Complex (NOCA). Their habitat requirements are quite specific and suitable habitat is patchily distributed across the landscape. During a11 seasons, mountain goat habitat is characterized by steep, rocky terrain. Summer habitat is generally above 1525 m (5000 ft) elevation, and features rock outcrops in or near subalpine meadows and forest (Welch, 1991; Holmes, 1993; Schoen and Kirchoff, 1981; NCASI, 1989; Chadwick, 1983; Benzon and Rice, 1988). Many mountain goat populations in Washington have declined during the last 20 years. Although specific causes have not been identified, several factors may have contributed to the regional decline. -
Geologic Map of Washington - Northwest Quadrant
GEOLOGIC MAP OF WASHINGTON - NORTHWEST QUADRANT by JOE D. DRAGOVICH, ROBERT L. LOGAN, HENRY W. SCHASSE, TIMOTHY J. WALSH, WILLIAM S. LINGLEY, JR., DAVID K . NORMAN, WENDY J. GERSTEL, THOMAS J. LAPEN, J. ERIC SCHUSTER, AND KAREN D. MEYERS WASHINGTON DIVISION Of GEOLOGY AND EARTH RESOURCES GEOLOGIC MAP GM-50 2002 •• WASHINGTON STATE DEPARTMENTOF 4 r Natural Resources Doug Sutherland· Commissioner of Pubhc Lands Division ol Geology and Earth Resources Ron Telssera, Slate Geologist WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES Ron Teissere, State Geologist David K. Norman, Assistant State Geologist GEOLOGIC MAP OF WASHINGTON NORTHWEST QUADRANT by Joe D. Dragovich, Robert L. Logan, Henry W. Schasse, Timothy J. Walsh, William S. Lingley, Jr., David K. Norman, Wendy J. Gerstel, Thomas J. Lapen, J. Eric Schuster, and Karen D. Meyers This publication is dedicated to Rowland W. Tabor, U.S. Geological Survey, retired, in recognition and appreciation of his fundamental contributions to geologic mapping and geologic understanding in the Cascade Range and Olympic Mountains. WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES GEOLOGIC MAP GM-50 2002 Envelope photo: View to the northeast from Hurricane Ridge in the Olympic Mountains across the eastern Strait of Juan de Fuca to the northern Cascade Range. The Dungeness River lowland, capped by late Pleistocene glacial sedi ments, is in the center foreground. Holocene Dungeness Spit is in the lower left foreground. Fidalgo Island and Mount Erie, composed of Jurassic intrusive and Jurassic to Cretaceous sedimentary rocks of the Fidalgo Complex, are visible as the first high point of land directly across the strait from Dungeness Spit. -
Wilderness Trip Planner
National Park Service North Cascades National Park Service Complex U.S. Department of the Interior Stephen Mather Wilderness An Enduring Legacy of Wilderness “[I]t is hereby declared to be the policy of the Congress to secure for the American people of present and future generations the benefits of an enduring resource of wilderness.” — Wilderness Act, 1964 The North Cascades National Park Complex includes 684,000 acres in three units: North Cascades National Park, Lake Chelan National Recre- ation Area, and Ross Lake National Recreation Area. Congress has designated 94% of the Complex as the Stephen Mather Wilderness. Today, as in the past, wilderness is an important part of every American’s story. People seek out wilderness for a variety of reasons: physical or mental challenge; solitude, renewal, or a respite from modern life; or as a place to find inspiration and to explore our heritage. What draws you to visit wilderness? The Stephen Mather Wilderness is at the heart of over two million acres of some of the wildest lands remaining, a place “where the earth and its community of life are untrammeled by man….” Untrammeled (meaning“free of restraint,” “unconfined”) captures the essence of wilderness: a place where the natural processes of the land prevail, and the developments of modern technological society are substantially unnoticeable. Here, we are visitors, but we also come home—to our natural heritage. It is a place to experience our past, and a place to find future respite. This is the enduring legacy of wilderness. To Hope, B.C. -
Lithology, Structure, Geochronology, and Tectonic Implications of the Spider Glacier Unit and Holden Assemblage, North Cascades, Washington
San Jose State University SJSU ScholarWorks Master's Theses Master's Theses and Graduate Research Spring 2020 Lithology, Structure, Geochronology, and Tectonic Implications of the Spider Glacier Unit and Holden Assemblage, North Cascades, Washington Colin Phillips San Jose State University Follow this and additional works at: https://scholarworks.sjsu.edu/etd_theses Recommended Citation Phillips, Colin, "Lithology, Structure, Geochronology, and Tectonic Implications of the Spider Glacier Unit and Holden Assemblage, North Cascades, Washington" (2020). Master's Theses. 5108. DOI: https://doi.org/10.31979/etd.wcje-w4t5 https://scholarworks.sjsu.edu/etd_theses/5108 This Thesis is brought to you for free and open access by the Master's Theses and Graduate Research at SJSU ScholarWorks. It has been accepted for inclusion in Master's Theses by an authorized administrator of SJSU ScholarWorks. For more information, please contact [email protected]. LITHOLOGY, STRUCTURE, GEOCHRONOLOGY AND TECTONIC IMPLICATIONS OF THE SPIDER GLACIER UNIT AND HOLDEN ASSEMBLAGE, NORTH CASCADES, WASHINGTON A Thesis Presented to The Faculty of the Department of Geology San José State University In Partial Fulfillment of the Requirements for the Degree Master of Science by Colin Phillips May 2020 © 2020 Colin Phillips ALL RIGHTS RESERVED ii The Designated Thesis Committee Approves the Thesis Titled LITHOLOGY, STRUCTURE, GEOCHRONOLOGY AND TECTONIC IMPLICATIONS OF THE SPIDER GLACIER UNIT AND HOLDEN ASSEMBLAGE, NORTH CASCADES, WASHINGTON by Colin Phillips APPROVED FOR -
USGS Scientific Investigations Map 2940, Sheet 2
Scientific Investigations Map 2940 U.S. Department of the Interior Prepared in cooperation with Washington State Division of Geology and Earth Resources, U.S. National Park Service, and U.S. Forest Service Sheet 2 of 2 U.S. Geological Survey Pamphlets accompany map 123° 122° 121° 120° 121° 120° basalt lavas VOLCANIC 122° 121° 120° 49° 48°30’ erupt to form ARC 122° 121° 120° Mount Spickard oceanic plate BRITISH COLUMBIA MID-OCEAN 49° NORTHWEST OKANOGAN Ross Lake Fault Zone (System) Dome Ptarmigan River RIDGE Old Guard Glacier Mount Vedder Straight Peak Spine WESTERN Peak Peak Pk 49° Mountatn CANADA 5 BLOCK Point Baker Jack Mtn ocean floor basalt sedimentary Mt Baker ROBINSON MOUNTAIN UNITED METHOW Pasayten MOUNT BAKER [MB] rocks early Tertiary and Late Le Conte Glacier Twin 2000 [RM] STATES 10 Cretaceous metamorphism Sisters Jack METHOW BLOCK Mount 1600 San Juan BELLINGHAM Baker Mtn Robinson Mountain 4 CONCRETE 2000 Islands OCEANIC OCEANIC SU CHELAN BLOCK Methow CRUST rigid mantle B CRUST CASCADE 48°30’ Gardner Mtn LITHOSPHERE Creek DU Skagit C Fault Sedro 9 T rigid mantle DOMAIN Concrete CONTINENTAL TWISP plastic mantle plastic mantle IO Wolley Winthrop N early Late Cretaceous LITHOSPHERE 6 melting zone CONTINENTAL Sauk older STEHEKIN Washington (source of igneous rocks) Z melting zone metamorphism sedimentary O (more igneous rocks) Entiat DARRINGTON 1600 Pass Twisp MANTLE N OKANOGAN Mount rocks E 1200 P sediments SYSTEM U Misch LAKE LOBE G River Stehekin metamorphic Glacier pillow basalt E Lake rocks forming D T River a Peak Stillaguamish rr Darrington River dikes in METAMORPHIC g Vinegar Mt CHELAN S Glacier Chelan to Fault Fault O Bonanza n early Late Cretaceous 1200 U Peak gabbro Fault Pilchuck Peak -D 48° GLACIER N ultramafic rock e and Early Creataceous D SAUK RIVER [SR] TWISP [T] 2 3 v WENATCHEE BLOCK 48° i metamorphism Ophiolite layering ls SUBDUCTED OCEAN PLATE M Monroe 8 DOMAIN (OCEANIC LITHOSPHERE) t CORE MONROE Skykomish n OLYMPIC River F Chelan Figure 3. -
Summary of Upper Skagit Watershed Fish and Wildlife Monitoring
Summary of Upper Skagit Watershed Fish and Wildlife Monitoring Technical Meeting, North Cascades National Park Service Complex headquarters (Sedro- Woolley, WA), April 11, 2008 Participants: Twenty scientists and managers (see attached list) from the US National Park Service (NPS), Washington Dept of Fish and Wildlife (WDFW); US Forest Service (FS); Seattle City Light (SCL); British Columbia Ministry of Environment (MOE); Skagit Environmental Endowment Commission (SEEC) Meeting objectives per the meeting agenda: • Sharing information on ongoing fish & wildlife monitoring projects within the Upper Skagit Watershed • Identifying opportunities for collaboration • Identifying needs/opportunities for data management • Linking monitoring projects to land management needs Presentation summaries (in order they were given): Jack Oelfke, North Cascades National Park Service Complex: Jack provided an overview of the NPS Inventory and Monitoring Program, a national program tailored to the local level that establishes the foundation and basis for a long-term biotic and abiotic ecological monitoring program in the park complex. Goals of the monitoring program include: building understanding of Park resources by tracking status and trends of key resource components; providing the basis for early warning about threats to Park resources; providing reference information useful for comparing resources in the Park to those in less well protected environments. After years of development the following monitoring projects (“Vital Signs”) will be implemented in the North Cascades NPS Complex: mountain lakes, subalpine-forest vegetation; landbirds; glaciers; climate; and landscape dynamics (remote sensing/aerial imagery). Funding limitations prohibit implementation of a broader range of Vital Signs at this time. The program has extensive database management, analysis, and reporting components to ensure long-term archival of information and availability to the public, managers, the research community, etc. -
East-Derived Strata in the Methow Basin Record Rapid Mid-Cretaceous Uplift of the Outhes Rn Coast Mountains Batholith Kathleen D
Trinity University Digital Commons @ Trinity Geosciences Faculty Research Geosciences Department 1-2014 East-derived Strata in the Methow Basin Record Rapid Mid-Cretaceous Uplift of the outheS rn Coast Mountains Batholith Kathleen D. Surpless Trinity University, [email protected] Zachary T. Sickmann Trinity University, [email protected] Trevor Koplitz Trinity University, [email protected] Follow this and additional works at: https://digitalcommons.trinity.edu/geo_faculty Part of the Earth Sciences Commons Repository Citation Surpless, K.D., Sickmann, Z.T., & Koplitz, T.A. (2014). East-derived strata in the Methow basin record rapid mid-Cretaceous uplift of the southern coast mountains Batholith. Canadian Journal of Earth Sciences, 51(4), 339-357. doi:10.1139/cjes-2013-0144 This Article is brought to you for free and open access by the Geosciences Department at Digital Commons @ Trinity. It has been accepted for inclusion in Geosciences Faculty Research by an authorized administrator of Digital Commons @ Trinity. For more information, please contact [email protected]. 339 ARTICLE East-derived strata in the Methow basin record rapid mid-Cretaceous uplift of the southern Coast Mountains batholith1 Kathleen D. Surpless, Zachary T. Sickmann, and Trevor A. Koplitz Abstract: The Jurassic–Cretaceous Methow basin of northern Washington State and southern British Columbia forms an overlap sequence linking several small tectonostratigraphic terranes. Sandstone petrography, sandstone and mudrock geochemistry, and detrital zircon U–Pb age -
1963 TERM Robert N
the Mountaineer 1964 Entered as second-class matter, April 8, 1922, at Post Office in Seattle, Wash., under the Act of March 3, 1879. Published monthly and semi-monthly during March and December by THE MOUNTAINEERS, P. 0. Box 122, Seattle 11, Wash. Clubroom is at 523 Pike Street in Seattle. Subscription price is $4.00 per year. Individual copies $2.00 each. The Mountaineers To explore and study the mountains, fores ts, 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 in fulfill ment of the above purposes; To encourage a spirit of good fellowship among all lovers of outdoor life. EDITORIAL STAFF Betty Manning, editor, Winifred Coleman, Peggy Ferber, Grace Kent, Nancy Miller, Marjorie Wilson The Mountaineers OFFICERS AND TRUSTEES 1963 TERM Robert N. Latz, President John F. Fuller, Secretary John Osseward, Vice-President Ed ward H. Murray, Treasurer Alvin Randall Frank Fickeisen El len Brooker Roy A. Snider Leo Gallagher John Klos Peggy Lawton Leon Uziel Harvey Manning J. D. Cockrell (Tacoma) Art Huffine Gr. Representative) Jon Hisey (Everett) OFFICERS AND TRUSTEES: TACOMA BRANCH Nels Bjarke, Chairman Marge Goodman, Treasurer Mary Fries, Vice-Chairman Steve Garrett Jack Gallagher Gr. Representative) Bruce Galloway Myrtle Connelly George Munday Helen Sohlberg, Secretary OFFICERS: EVERETT BRANCH Larry Sebring, Chairman Glenda Bean, Secretary Gail Crummett, Treasurer COPYRIGHT 1964 BY THE MOUNTAINEERS The Mountaineer Climbing Code A climbing party of three is the minimum, unless adequate sup port is available from those who have knowledge that the climb is in progress. -
North Cascades
S k a g North CHILLIWACK i To Hope, BC t 40mi 64km SKAGIT VALLEY R MANNING i 0 5 Kilometers LAKE v e r Silver-Skagit PROVINCIAL PARK PROVINCIAL PARK PROVINCIAL Road 0 5 Miles PARK British Columbia Ross Lake CANADA Washington Hozomeen UNITED STATES S i Silver Hozomeen Mountain Mount Winthrop le Sil Ho Castle Peak s ve zo 8066ft 7850ft Lake r m 8306ft ia STEPHEN MATHER C re e 2459m 2532m 2393m ek e Little Jackass n MOUNT BAKER WILDERNESS C Mount Spickard r Mountain T e WILDERNESS Be 8979ft r e a 4387ft a k r Mount Redoubt R 2737m Hozomeen e i Castle d 1337m l C 8969ft o l u Lake i re 2734m bt G Pass a e la r k cie r 4-wheel-drive T P W e r Ridley Lake conditions east ry il Joker k Twin R Jack lo of this point c w Mountain a e k Lakes Point L ree C 7603ft d R C w ak rail i Copper Mountain r e T n l Willow r o O 2317m e il l Bear Mountain e e k 7142ft a i e t r v u C le n h T 7932ft e re S Lake e t F Hopkins i b e s a 2177m C o k e w R 2418m k S a Pass t r r u To Glacier e C k Goat Mountain g h I C c (US Forest Service and d n u 6890ft i d h National Park Service R k i C 2100m c a See State Route 20 Detail Below information) a n 4mi 6km r iw n e ll rail Skagit Peak Natio al p i aver T Desolation st S p h Cree tle Be 6800ft P we ce o C k Lit Peak Do not use this map for a h n C 2073m k Noo ci t i 6102ft e k 542 fi r c k backcountry hiking.