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United States Department of the Interior U.S. Geological Survey
UNITED STATES DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY RESOURCE ASSESSMENT OF THE BUREAU OF LAND MANAGEMENT'S WINNEMUCCA DISTRICT AND SURPRISE RESOURCE AREA, NORTHWEST NEVADA AND NORTHEAST CALIFORNIA An Interim Project Status Report by Jeff L. Doebrich \ George V. Albino 2, Charles E. Barker 3, Wendell A. Duffield 4, Victor C. Dunn s, Willam F. Hanna 6, Joseph P. McFarlan 7, Dawn J. McGuire 8, Michael S. Miller 9, Stephen G. Peters \ Donald Plouff 10, Gary L. Raines \ Don L. Sawatzky1, and Gregory T. Spanski " United States Geological Survey Open-File Report 94-712 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards or with the North America Stratigraphic Code. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. 1994 'USGS, MS 176, Reno Field Office, Mackay School of Mines, University of Nevada, Reno, NV 89557-0047 2U.S. Geological Survey, Unit 62101, APO AE 09811-2101 3USGS, MS 971, Box 25046, Denver Federal Center, Denver, CO 80225-0046 4USGS, Bldg. 3, 2255 North Gemini Dr., Flagstaff, AZ 86001-1698 5Bureau of Land Management, 705 E. 4th St., Winnemucca, NV 89445 6USGS, National Center, MS 927, 12201 Sunrise Valley Dr., Reston, VA 22092-0001 7Bureau of Land Management, P.O. Box 460, Cedarville, CA 96104 8USGS, MS 973, Box 25046, Denver Federal Center, Denver, CO 80225-0046 'Western Field Operations Center, U.S. Bureau of Mines, E. 360 Third Ave., Spokane, WA 99202 10USGS, MS 989, Bldg. -
Clyde Wahrhaftig Collection
Clyde Wahrhaftig Collection GOGA 35329 Golden Gate National Recreation Area Park Archives and Records Center ATTN: Park Archives and Records Center Presidio of San Francisco Building 201, Fort Mason Building 667 McDowell Ave. San Francisco, CA 94123 San Francisco, CA 94129 [Mailing Address] [Physical Address] go.nps.gov/gogacollections Phone: 415-561-2807 Fax: 415-441-1618 Introduction Golden Gate National Recreation Area Park Description Golden Gate National Recreation Area (GGNRA), a unit of the National Park Service, was established by an Act of Congress on October 27, 1972. The 80,000-acre park encompasses a great diversity of cultural and natural resources in and around the Bay Area of San Francisco, California. It includes Muir Woods National Monument and Fort Point National Historic Site. The park holds almost five million three-dimensional and documentary artifacts dating from the time before European contact to the present. They are preserved and maintained for the public by the Division of Cultural Resources and Museum Management, which includes the Park Archives and Records Center (PARC). Park Archives and Records Center (PARC) Historical Note GGNRA and the sites within it have been collecting records since their inception. The PARC was established in 1994 to receive records and archival collections from the U.S. Army and the Presidio Army Museum after the closure of the Presidio of San Francisco as an Army base. The collections continue to grow through the donation of materials by private individuals, transfer of inactive park records by staff, and acquisition of relevant documentary materials. Scope of Collections The archival collections in the custody of the GGNRA document the history and activity of the various sites and groups associated with the park, described in the park’s Scope of Collection Statement (2009). -
MOUNTAINEERS.Orgmountaineerspring 2019 • VOLUME 113 • NO
WWW.MOUNTAINEERS.ORGMountaineerSpring 2019 • VOLUME 113 • NO. 2 EXPLORE • LEARN • CONSERVE in this issue: Three Generations Outside The Baby Peakbagger Confessions of an Old Scrambling Student tableofcontents tyingin Features The Mountaineers is a nonprofit 20 The Baby Peakbagger As CEO of The Mountaineers I have the organization, founded in 1906 Spring 2019 » Volume 113 » Number 2 Exploring Mount Rainier National Park with my daughter opportunity to attend many events across and dedicated to the responsible The Mountaineers enriches lives and communities by the organization throughout the year. One enjoyment and protection of natural areas. helping people explore, conserve, learn about, and enjoy 24 Three Generations Outside of my very favorite events is our Volunteer A love letter to my sons and granddaughters the lands and waters of the Pacific Northwest and beyond. Recognition Dinner, which takes place in EDITOR 30 Confessions of an Old Scrambling Student January. I love this event because it celebrates Peter Dunau Using mountains to take on aging the creativity, hard work, and commitment of CONTRIBUTING EDITOR our incredible volunteers. Kristina Ciari 39 A New Program Center for our Kitsap Branch DESIGNER For me, and most everyone who volunteers Opportunities abound in revamped building Sarah Kulfan, Beans n' Rice at The Mountaineers, volunteering is a way of PROOFREADERS sharing the joy of being outdoors with others. Trevor Dickie, Elaine Kelly, Hailey Oppelt Columns Tom and sons on Mt. Rainier We volunteer as an act of love for our wild CHIEF EXECUTIVE OFFICER 5 READER FEEDBACK places and out of gratitude for those who Tom Vogl introduced us to a lifetime of outdoor adventure. -
Paleotectonic Investigations of the Permian System in the United States
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Publications of the US Geological Survey US Geological Survey 1967 Paleotectonic Investigations of the Permian System in the United States Edwin D. McKee Stephen S. Oriel Henry L. Berryhill Eleanor J. Crosby Donald A. Myers See next page for additional authors Follow this and additional works at: https://digitalcommons.unl.edu/usgspubs Part of the Geochemistry Commons, Geology Commons, Geomorphology Commons, Hydrology Commons, and the Other Earth Sciences Commons This Article is brought to you for free and open access by the US Geological Survey at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Publications of the US Geological Survey by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. Authors Edwin D. McKee, Stephen S. Oriel, Henry L. Berryhill, Eleanor J. Crosby, Donald A. Myers, George H. Dixon, Marjorie E. MacLachlan, Melville R. Mudge, Edwin K. Maughan, Richard P. Sheldon, Earl R. Cressman, Thomas M. Cheney, Walter E. Hallgarth, and Keith B. Ketner Paleotectonic Investigations of the Permian System in the United States GEOLOGICAL SURVEY PROfESSIONAL PAPER 515 w- PALEOTECTONIC INVESTIGATIONS OF THE PERMIAN SYSTEM IN THE UNITED STATES RECONSTRUCTION OF SEASCAPE IN GLASS MOUNTAIN AREA, BREWSTER COUNTY, TEXAS, DURING MIDDLE PART (LEONARD) OF PERMIAN TIME The reconstruction is based on a diorama prepared by George Marchard for the U- S National Museum. Technical assistance for the reconstruction was fur nished by G. Arthur Cooper and G. Edward Lewis. Paleotectonic Investigations of the Permian System in the United States By E. D. McKEE, S. S. ORIEL, and others GEOLOGICAL SURVEY PROFESSIONAL PAPER 515 UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1967 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. -
Allan Cox Papers SC0343
http://oac.cdlib.org/findaid/ark:/13030/kt0r29r89t No online items Guide to the Allan Cox Papers SC0343 Daniel Hartwig & Jenny Johnson Department of Special Collections and University Archives October 2010 Green Library 557 Escondido Mall Stanford 94305-6064 [email protected] URL: http://library.stanford.edu/spc Note This encoded finding aid is compliant with Stanford EAD Best Practice Guidelines, Version 1.0. Guide to the Allan Cox Papers SC034315385 1 SC0343 Language of Material: English Contributing Institution: Department of Special Collections and University Archives Title: Allan Cox papers Creator: Cox, Allan Identifier/Call Number: SC0343 Identifier/Call Number: 15385 Physical Description: 20.75 Linear Feet Date (inclusive): 1954-1987 Abstract: Papers document his professional life as teacher, administrator, and researcher and include correspondence; memoranda; research notes, charts, proposals, and reports; grant applications; outlines, tests, lecture notes, and other teaching materials; manuscripts; minutes; date books; papers and theses by his students; reprints; maps; and his notes while a student at UC Berkeley. Cox studied paleomagnetism and plate tectonics theory; some materials pertain to research done on the Galapagos Islands and in China. Information about Access This collection is open for research. Ownership & Copyright All requests to reproduce, publish, quote from, or otherwise use collection materials must be submitted in writing to the Head of Special Collections and University Archives, Stanford University Libraries, Stanford, California 94304-6064. Consent is given on behalf of Special Collections as the owner of the physical items and is not intended to include or imply permission from the copyright owner. Such permission must be obtained from the copyright owner, heir(s) or assigns. -
Memorial to Clyde Wahrhaftig 1919-1994 GARNISS H
Memorial to Clyde Wahrhaftig 1919-1994 GARNISS H. CURTIS Berkeley Geochronology Center, University o f California Berkeley, California 94709 Clyde Wahrhaftig was born in Fresno, California, on December 1, 1919. He died on April 6, 1994, of heart failure. Reared in Fresno in a pioneer California family who had started many of the orchards in the Sacramento Valley, he was introduced to Berkeley at an early age on family vacations when his mother attended classes at the Univer sity of California, and he felt always that this was his true home. Strawberry Creek and the hills in back of the UC campus were his playground. Later, when he joined the staff at the UC Department of Geology and Geophysics in 1960, he taught field classes in those beloved hills. Clyde received a bachelor’s degree in geology from the California Institute of Technology in 1941, and a Ph.D. in geology from Harvard University in 1953. He worked full-time for the U.S. Geological Survey from 1941 until 1960, when he joined the UC Berkeley faculty, part-time from 1960 until he retired from UC Berkeley in 1982, and again full-time until his death in 1994. Most of his professional work with the Survey was in Alaska, much of it concerned with coal deposits; but at various times he studied many aspects of Alaskan geology in areas ranging from the Brooks Range to the north to the Kuskoquim Mountains and the Alaska Range to the south. Some of these studies remained unfinished at the time of his death. -
Bedrock Geologic Map of Yosemite Valley, Yosemite National Park, California
: I / DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY L, BEDROCK GEOLOGIC MAP OF YOSEMITE VALLEY, YOSEMITE NATIONAL PARK, CALIFORNIA By Frank C. Calkins and others MISCELLANEOUS N,IVESTIGATONS SERIES Published by the U.S. Geological Survey, 1985 G DEPARTMENT OF THE INTERIOR TO ACCOMPAI{Y MAP I-1639 U.S, GEOLOGICAL SURVEY BEDROCK GEOLOGY OF THE YOSEMITE VALLEY AREA YOSEMITE NATIONAL PARK, CALIFORNIA Prepared by N. King Huber and Julte A. Roller From the wrttlngs of Frank C. Calklns and other sources PREFACE INTRODUCTION Frank Calkins' work in Yosemite was preceded by Yosemite Valley, one of the world's great natural works Henry W. Tumer, also of the U.S. Geological Survey, of rock sculpfure, is carved into the west slope of the who began mapping the Yosemite and Mount Lyell 30- Siena Nevada. Immense cliffs, domes, and waterfalls minute quadrangles in 1897 and laid the foundation that tower over forest, meadows, and a meandering river, Calkins' work was built on. Although Tumer never creating one of the most scenic nafural landscapes in completed this sizable assignment, he recognized the North America (fig. 1). In Yosemite Valley and the differing types oI plutonic rocks and, for example, named adloining uplands, the forces of erosion have exposed, the El Capitan Granite. with exceptional clarity, a highly complex assemblage of Calkins mapped the valley and adjacent areas of granitic rocks. The accompanying geologc map shows the Yosemite National Park during the period 1913 through distibution of some of the different rocks that make up 1916, at the same time that Francois Matthes was this assemblage. -
Geology of Northern California : Field Trip
NOTICE CONCERNING COPYRIGHT RESTRICTIONS This document may contain copyrighted materials. These materials have been made available for use in research, teaching, and private study, but may not be used for any commercial purpose. Users may not otherwise copy, reproduce, retransmit, distribute, publish, commercially exploit or otherwise transfer any material. The copyright law of the United States (Title 17, United States Code) governs the making of photocopies or other reproductions of copyrighted material. Under certain conditions specified in the law, libraries and archives are authorized to furnish a photocopy or other reproduction. One of these specific conditions is that the photocopy or reproduction is not to be "used for any purpose other than private study, scholarship, or research." If a user makes a request for, or later uses, a photocopy or reproduction for purposes in excess of "fair use," that user may be liable for copyright infringement. This institution reserves the right to refuse to accept a copying order if, in its judgment, fulfillment of the order would involve violation of copyright law. GEOLOGY OF THE SIERRA NEVADA By Paul C. Bateman and Clyde Wahrhaftig * U.S. Geological Survey, Menlo Park, California; U.S.G.S. AND University of California, Berkeley The Sierra Nevada is a strongly asymmetric moun- tending south from the Cascade Range. A blanket of tain range with a long gentle \\estern slope and a high volcanic material caps large areas in the north part of and steep eastern escarpment. It is 50 to 80 miles wide, the range. and it runs west of north through eastern California Most of the south half of the Sierra Nevada and the for more than 400 miles—from the Mojave Desert on eastern part of the north half are composed of plutonic the south to the Cascade Range and the Modoc Plateau (chiefly granitic) rocks of Mesozoic age. -
Text-Only PDF File
Geological Field Trips in Southern Idaho, Eastern Oregon, and Northern Nevada Edited by Kathleen M. Haller, and Spencer H. Wood Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government Open-File Report 2004-1222 U.S. Department of the Interior U.S. Geological Survey Geological Field Trips in Southern Idaho, Eastern Oregon, and Northern Nevada Edited by Kathleen M. Haller, and Spencer H. Wood Contents Introduction ...................................................................................................................................................... 2 The Rattlesnake Tuff and Other Miocene Silicic Volcanism in Eastern Oregon By Martin Streck and Mark Ferns ....................................................................................................... 4 The Western Margin of North America After the Antler Orogeny: Mississippian Through Late Permian History in the Basin and Range, Nevada By James H. Trexler, Jr., Patricia H. Cashman, Walter S. Snyder, and Vladimir I. Davydov......... 20 Fire and Ice in Central Idaho: Modern and Holocene Fires, Debris Flows, and Climate in the Payette River Basin, and Quaternary and Glacial Geology in the Sawtooth Mountains By Jennifer L. Pierce, Grant A. Meyer, Glenn D. Thackray, Spencer H. Wood, Kari Lundeen, Jennifer A. Borgert, and Eric Rothwell............................................................................... 38 Late-Pleistocene Equilibrium-Line Altitudes, Atmospheric Circulation, and Timing of Mountain -
Stable Isotopes Analysis of Caribou Antlers As Ecological Indicators
Stable Isotopes Analysis of Caribou Antlers as Ecological Indicators By Matthew Brenning A Thesis submitted to the Faculty of Graduate and Postdoctoral Affairs in partial fulfillment of the requirements for the degree of Master of Science In Earth Science Carleton University Ottawa, Ontario ©2020 Matthew Brenning Abstract This study aims to determine whether Rangifer tarandus (caribou) antlers provide a unique isotopic signal relative to other hard tissues such as bone and teeth using stable isotopes of oxygen, carbon, and nitrogen. Variation in the rate and timing of tissue development should create different stable isotope profiles for each tissue. Tissue from fifteen male specimens housed at the Canadian Museum of Nature were sampled. Stable isotope analysis was conducted along the length of the antler, on the third molar, and the mandible. Isotopic differences were found between the three tissues, with the carbonate carbon (δ13C) and collagen nitrogen (δ15N) isotopes showing significant patterns of variation along the length of the antlers. Isotopic variation along the antler length could potentially reflect ecological or physiological changes within the male caribou. Addition testing with plant samples, including mixing models with antler values, may provide deeper insight into this isotopic variation. ii Acknowledgements Dr. Danielle Fraser is an outstanding supervisor, she has provided me with support both in the lab and on the page. I am so grateful that I have had such an encouraging mentor in my corner. I would not have been able to complete this project without her and I owe so much of this thesis to her. I would also like to acknowledge my amazing committee who have been both teachers and critics helping me shape this project. -
Washington Geology, V. 19, No. 3, October 1991
WASHINGTON GEOLOGY formerly WASHINGTON GEOLOGIC NEWSLETTER Washington Department of Natural Resources, Division of Geology and Earth Resources Vol. 19, No. 3, Oct. 1991 Seattle was the site of the First International Symposium on Volcanic Ash and Aviation Safety this July, which devoted a special session to the Pinatubo volcano eruption in the Philippines. Shown here is a view of the June 12 eruption column as seen from Clark Air Base, 20 km east-northeast of Pinatubo. Photograph by Robert S. Culbreth. In This Issue: Geologic guide for State Routes 240 and 243 in south-central Washington, p. 3; Significance of the Eocene fossil plants at Republic, Washington, p. 18; Highlights of the Volcanic Ash and Aviation Safety Symposium, p. 25; USSR trip promotes exchange of seismic information, p. 30; 1991 geological projects, Washington colleges and universities, p. 33. Sunrise Review of the Practice of Geology WASHINGTON (18.118 RCW) GEOLOGY Executive Summary In 1989, legislation (SHB 1597) was enacted that required a sunrise review of the practice of geology in Washington Geology (formerly the Washington Geologic Washington State. State policy as delineated under Newsletter) is published four times a year by the Washington 18.118 RCW makes it clear that additional regulation Division of Geology and Earth Resources, Department of Natural Resources. This publication is free upon request. The Division of business professions be imposed only In those cases also publishes bulletins, information circulars, reports of investi where such regulation Is necessary to protect the In gations, geologic maps, and open-file reports. A list of these terests of the public. -
CLYDE WAHRHAFTIG Dept. Geology and Geophysics, University of California, Berkley, California
CLYDE WAHRHAFTIG Dept. Geology and Geophysics, University of California, Berkley, California Stepped Topography of the Southern Sierra Nevada, California Abstract: Irregular steps characterize the topogra- much more rapid weathering of granitic rocks where phy on granitic terrane on the west slope of the buried than where exposed. Weathering is predomi- southern Sierra Nevada. These steps are a few nantly by partial alteration and expansion of biotite, hundred leet to a few thousand feet high, one- which shatters the rock. The disintegrated rock can quarter to 5 miles wide, and up to 10 miles long. be moved readily by small streams. The unweath- Most steps face the San Joaquin Valley, but others ered outcrops exposed by accelerated erosion act as line the canyons of the major rivers, facing the local baselevels, because their large joint blocks can- streams. Part of the eastern edge of the San Joaquin not be moved by even the largest streams. Valley is a smooth plain bevelled across granite, and Alternative hypotheses include faulting, differ- has an origin similar to the steps. Outcrops are com- ential erosion due to variations in bedrock lithology mon on the fronts of the steps, and near the outer or in spacing of joints, and parallel retreat of the edges of the step treads, but are rare on the back fronts, with the treads aspiedmonttreppen. Evidence parts oi the treads, which are underlain by disinte- is presented that renders each of these hypotheses grated granitic rock as much as 100 feet thick. doubtful. Treads tend to slope back toward the next higher The proposed hypothesis raises questions about front.