Antarctic Meteorite Location and Mapping Project
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University Microfilms, Inc., Ann Arbor, Michigan GEOLOGY of the SCOTT GLACIER and WISCONSIN RANGE AREAS, CENTRAL TRANSANTARCTIC MOUNTAINS, ANTARCTICA
This dissertation has been /»OOAOO m icrofilm ed exactly as received MINSHEW, Jr., Velon Haywood, 1939- GEOLOGY OF THE SCOTT GLACIER AND WISCONSIN RANGE AREAS, CENTRAL TRANSANTARCTIC MOUNTAINS, ANTARCTICA. The Ohio State University, Ph.D., 1967 Geology University Microfilms, Inc., Ann Arbor, Michigan GEOLOGY OF THE SCOTT GLACIER AND WISCONSIN RANGE AREAS, CENTRAL TRANSANTARCTIC MOUNTAINS, ANTARCTICA DISSERTATION Presented in Partial Fulfillment of the Requirements for the Degree Doctor of Philosophy in the Graduate School of The Ohio State University by Velon Haywood Minshew, Jr. B.S., M.S, The Ohio State University 1967 Approved by -Adviser Department of Geology ACKNOWLEDGMENTS This report covers two field seasons in the central Trans- antarctic Mountains, During this time, the Mt, Weaver field party consisted of: George Doumani, leader and paleontologist; Larry Lackey, field assistant; Courtney Skinner, field assistant. The Wisconsin Range party was composed of: Gunter Faure, leader and geochronologist; John Mercer, glacial geologist; John Murtaugh, igneous petrclogist; James Teller, field assistant; Courtney Skinner, field assistant; Harry Gair, visiting strati- grapher. The author served as a stratigrapher with both expedi tions . Various members of the staff of the Department of Geology, The Ohio State University, as well as some specialists from the outside were consulted in the laboratory studies for the pre paration of this report. Dr. George E. Moore supervised the petrographic work and critically reviewed the manuscript. Dr. J. M. Schopf examined the coal and plant fossils, and provided information concerning their age and environmental significance. Drs. Richard P. Goldthwait and Colin B. B. Bull spent time with the author discussing the late Paleozoic glacial deposits, and reviewed portions of the manuscript. -
Office of Polar Programs
DEVELOPMENT AND IMPLEMENTATION OF SURFACE TRAVERSE CAPABILITIES IN ANTARCTICA COMPREHENSIVE ENVIRONMENTAL EVALUATION DRAFT (15 January 2004) FINAL (30 August 2004) National Science Foundation 4201 Wilson Boulevard Arlington, Virginia 22230 DEVELOPMENT AND IMPLEMENTATION OF SURFACE TRAVERSE CAPABILITIES IN ANTARCTICA FINAL COMPREHENSIVE ENVIRONMENTAL EVALUATION TABLE OF CONTENTS 1.0 INTRODUCTION....................................................................................................................1-1 1.1 Purpose.......................................................................................................................................1-1 1.2 Comprehensive Environmental Evaluation (CEE) Process .......................................................1-1 1.3 Document Organization .............................................................................................................1-2 2.0 BACKGROUND OF SURFACE TRAVERSES IN ANTARCTICA..................................2-1 2.1 Introduction ................................................................................................................................2-1 2.2 Re-supply Traverses...................................................................................................................2-1 2.3 Scientific Traverses and Surface-Based Surveys .......................................................................2-5 3.0 ALTERNATIVES ....................................................................................................................3-1 -
Rb-Sr Provenance Dates of Feldspar in Glacial Deposits of the Wisconsin Range, Transantarctic Mountains
Rb-Sr provenance dates of feldspar in glacial deposits of the Wisconsin Range, Transantarctic Mountains q F/XUR.E ' I Department of Geology and Mineralogy and Institute of Polar Studies, The Ohio State University, Columbus, J H MERCER ' °hi°43210 ABSTRACT than those of feldspar in the plateau till and range only from 0.46 to 0.66. Nevertheless, three feldspar fractions form a straight line on Glacial deposits in the Wisconsin Range (lat. 85° to 86°30'S, the Rb-Sr isochron diagram, the slope of which indicates a date of long. 120° to 130°W) of the Transantarctic Mountains include a 576 ± 21 Ma. The difference in the date derived from the feldspar of deposit of till on the summit plateau at an elevation of 2,500 m the glaciolacustrine sedimeyt may be caused by the presence of a above sea level and glaciolacustrine sediments along the Reedy component of Precambrian feldspar derived from the East Antarc- Glacier. The plateau till and underlying sediments consist of six tic Shield. units that appear to record the replacement of ice-free, periglacial conditions by ice cap glaciation of pre-Pleistocene age. Alterna- INTRODUCTION tively, the plateau till may have been deposited by the East Antarc- tic ice sheet either when it was thicker than at present or when the The glaciation of Antarctica in Cenozoic time was an important Wisconsin Range was lower in elevation. Feldspar size fractions event in the history of the Earth, the effects of which continue to from the plateau till have Rb/Sr ratios that increase with grain size influence climatic conditions and sea level. -
Read Ebook {PDF EPUB} on the Run by Jacklyn Dumais on the Run by Jacklyn Dumais
Read Ebook {PDF EPUB} On the Run by Jacklyn Dumais On the Run by Jacklyn Dumais. Completing the CAPTCHA proves you are a human and gives you temporary access to the web property. What can I do to prevent this in the future? If you are on a personal connection, like at home, you can run an anti-virus scan on your device to make sure it is not infected with malware. If you are at an office or shared network, you can ask the network administrator to run a scan across the network looking for misconfigured or infected devices. Another way to prevent getting this page in the future is to use Privacy Pass. You may need to download version 2.0 now from the Chrome Web Store. Cloudflare Ray ID: 660fafe0fbc018e5 • Your IP : 116.202.236.252 • Performance & security by Cloudflare. On the Run by Jacklyn Dumais. Completing the CAPTCHA proves you are a human and gives you temporary access to the web property. What can I do to prevent this in the future? If you are on a personal connection, like at home, you can run an anti-virus scan on your device to make sure it is not infected with malware. If you are at an office or shared network, you can ask the network administrator to run a scan across the network looking for misconfigured or infected devices. Another way to prevent getting this page in the future is to use Privacy Pass. You may need to download version 2.0 now from the Chrome Web Store. -
The Stratigraphy of the Ohio Range, Antarctica
This dissertation has been 65—1200 microfilmed exactly as received LONG, William Ellis, 1930- THE STRATIGRAPHY OF THE OHIO RANGE, ANTARCTICA. The Ohio State University, Ph.D., 1964 G eology University Microfilms, Inc., Ann Arbor, Michigan THE STRATIGRAPHY OF THE OHIO RANGE, ANTARCTICA DISSERTATION Presented in Partial Fulfillment of the Requirements for the Degree Doctor of Philosophy in the Graduate School of The Ohio State University By William Ellis Long, B.S., Rl.S. The Ohio State University 1964 Approved by A (Miser Department of Geology PLEASE NOTE: Figure pages are not original copy* ' They tend tc "curl11. Filled in the best way possible. University Microfilms, Inc. Frontispiece. The Ohio Range, Antarctica as seen from the summit of ITIt. Glossopteris. The cliffs of the northern escarpment include Schulthess Buttress and Darling Ridge. The flat area above the cliffs is the Buckeye Table. ACKNOWLEDGMENTS The preparation of this paper is aided by the supervision and advice of Dr. R. P. Goldthwait and Dr. J. M. Schopf. Dr. 5. B. Treves provided petrographic advice and Dir. G. A. Doumani provided information con cerning the invertebrate fossils. Invaluable assistance in the fiBld was provided by Mr. L. L. Lackey, Mr. M. D. Higgins, Mr. J. Ricker, and Mr. C. Skinner. Funds for this study were made available by the Office of Antarctic Programs of the National Science Foundation (NSF grants G-13590 and G-17216). The Ohio State Univer sity Research Foundation and Institute of Polar Studies administered the project (OSURF Projects 1132 and 1258). Logistic support in Antarctica was provided by the United States Navy, especially Air Development Squadron VX6. -
Lower Devonian), Ohio Range, Transantarctic Mountains GEORGIA TECH L=ARY
7 87-670,P 6.000046'24 —tt'Vt.t.tt 4 GEORGIA TECH LIBRAR. Petrology and Sedimentology of the Horlick Formation (Lower Devonian), Ohio Range, Transantarctic Mountains GEORGIA TECH L=ARY NOV 181 'f.ki TS GRY st-Cr ,1M U.S. GEOLOGICAL SURVEY BULLETIN 1780 GEORGIA JECH Libtspir.1 Petrology and Sedimentology of the Horlick Formation (Lower Devonian), Ohio Range, Transantarctic Mountains By LUCY McCARTAN and MARGARET A. BRADSHAW The Horlick Formation is a nearshore marine deposit of fossiliferous sandstone and shale; it is the oldest sedimentary formation in the Ohio Range GEORGIA TECH LIBRARY NOV 1 8 1117 DCUMLiS 9EPOSIT Gift t. ? U.S. GEOLOGICAL SURVEY BULLETIN 1780 DEPARTMENT OF THE INTERIOR DONALD PAUL HODEL, Secretary U.S. GEOLOGICAL SURVEY Dallas L. Peck, Director UNITED STATES GOVERNMENT PRINTING OFFICE: 1987 For sale by the Books and Open-File Reports Section, U.S. Geological Survey, Federal Center, Box 25425, Denver, CO 80225 Library of Congress Cataloging in Publication Data McCartan, Lucy. Petrology and sedimentology of the Horlick Formation (Lower Devonian), Ohio Range, Transantarctic Mountains. (U.S. Geological Survey bulletin ; 1780) Bibliography: p. Supt. of Docs. no.: I 19.3:1780 1.Sandstone—Antarctic regions—Transantarctic Mountains. 2. Shale—Antarctic regions—Transantarctic Mountains. 3. Sedimentation and deposition—Antarctic regions— Transantarctic Mountains. 4. Geology, Stratigraphic— Devonian. 5. Geology—Antarctic regions—Transantarctic Mountains. I. Bradshaw, Margaret A. II. Title. III. Series. QE75.B9 no. 1780 557.3 s -
Blue Ice Runway Site Survey, Pensacola Mountains
Blue ice runway site survey, Jy Pensacola Mountains - Hanmih 6 AuggIt Brown ak Nunatak Walket Pk A. KOVACS and G. ABELE U.S. Army Cold Regions Research and Engineering Laboratory Hanover, New Hampshire 03755 From January 19 to January 30, 1974, a U.S. Army Cold Regions Research and Engineering Laboratory (cIuEL) field party conducted a survey of potential j I /i I ( runway sites for heavy, wheeled airplane (e.g. C-130, j ; L C-141. and C-5A) landings in the Pensacola Moun- tains. The major emphasis was on finding a large area of blue glacial ice that could, with very little prepara- tion, be used for wheeled aircraft landings. The need for such a runway is predicated on future logistics requirements of research programs in the Pensacola Mountains, and of an analysis of overall Y .J rRDNR U.S. antarctic logistics support operations (Day et al., rail Pk 1973). This analysis shows that money could be \ 3O± saved by flying personnel and cargo in large, wheeled airplanes, to the Pensacola Mountains area (via the E A K S Antarctic Peninsula) ; from there, the Personnel and iackson i090_ - cargo would be transported to such stations as South F Pole and Siple in smaller, ski-equipped airplanes. En route to the put-in site (Cordiner Peaks), aerial reconnaissance of potential runway sites was made in the Patuxent Range, the Neptune Range, and the Cordirier Peaks. Weather conditions did not permit Figure 2. Traverse routes and mountain peaks climbed in the Cordiner Peaks. The black square at the bottom is put-in site an aerial reconnaissance of the Forrestal Range or location. -
The Transantarctic Mountains These Watercolor Paintings by Dee Molenaar Were Originally Published in 1985 with His Map of the Mcmurdo Sound Area of Antarctica
The Transantarctic Mountains These watercolor paintings by Dee Molenaar were originally published in 1985 with his map of the McMurdo Sound area of Antarctica. We are pleased to republish these paintings with the permission of the artist who owns the copyright. Gunter Faure · Teresa M. Mensing The Transantarctic Mountains Rocks, Ice, Meteorites and Water Gunter Faure Teresa M. Mensing The Ohio State University The Ohio State University School of Earth Sciences School of Earth Sciences and Byrd Polar Research Center and Byrd Polar Research Center 275 Mendenhall Laboratory 1465 Mt. Vernon Ave. 125 South Oval Mall Marion, Ohio 43302 Columbus, Ohio 43210 USA USA [email protected] [email protected] ISBN 978-1-4020-8406-5 e-ISBN 978-90-481-9390-5 DOI 10.1007/978-90-481-9390-5 Springer Dordrecht Heidelberg London New York Library of Congress Control Number: 2010931610 © Springer Science+Business Media B.V. 2010 No part of this work may be reproduced, stored in a retrieval system, or transmitted in any form or by any means, electronic, mechanical, photocopying, microfilming, recording or otherwise, without written permission from the Publisher, with the exception of any material supplied specifically for the purpose of being entered and executed on a computer system, for exclusive use by the purchaser of the work. Cover illustration: A tent camp in the Mesa Range of northern Victoria Land at the foot of Mt. Masley. Printed on acid-free paper Springer is part of Springer Science+Business Media (www.springer.com) We dedicate this book to Lois M. Jones, Eileen McSaveny, Terry Tickhill, and Kay Lindsay who were the first team of women to conduct fieldwork in the Transantarctic Mountains during the 1969/1970 field season. -
Comparing Numerical Ice-Sheet Model Output with Radio-Echo Sounding Measurements in the Weddell Sea Sector of West Antarctica
Annals of Glaciology Comparing numerical ice-sheet model output with radio-echo sounding measurements in the Weddell Sea sector of West Antarctica Hafeez Jeofry1,2 , Neil Ross3 and Martin J. Siegert1 Article 1Grantham Institute and Department of Earth Science and Engineering, Imperial College London, London Cite this article: Jeofry H, Ross N, Siegert MJ SW7 2AZ, UK; 2Faculty of Science and Marine Environment, Universiti Malaysia Terengganu, Kuala Terengganu (2020). Comparing numerical ice-sheet model 21300 Terengganu, Malaysia and 3School of Geography, Politics and Sociology, Newcastle University, Newcastle output with radio-echo sounding upon Tyne NE1 7RU, UK measurements in the Weddell Sea sector of West Antarctica. Annals of Glaciology 61(81), 188–197. https://doi.org/10.1017/aog.2019.39 Abstract Received: 24 July 2019 Numerical ice-sheet models are commonly matched to surface ice velocities from InSAR mea- Revised: 31 October 2019 surements by modifying basal drag, allowing the flow and form of the ice sheet to be simulated. Accepted: 31 October 2019 Geophysical measurements of the bed are rarely used to examine if this modification is realistic, First published online: 28 November 2019 however. Here, we examine radio-echo sounding (RES) data from the Weddell Sea sector of West Key words: Antarctica to investigate how the output from a well-established ice-sheet model compares with Ice-sheet modelling; ice streams; radio-echo measurements of the basal environment. We know the Weddell Sea sector contains the Institute, sounding Möller and Foundation ice streams, each with distinct basal characteristics: Institute Ice Stream lies partly over wet unconsolidated sediments, where basal drag is very low; Möller Ice Stream lies Author for correspondence: Martin J. -
Cosmogenic-Nuclide Exposure Ages from the Pensacola Mountains Adjacent to the Foundation Ice Stream, Antarctica
[American Journal of Science, Vol. 316, June, 2016,P.542–577, DOI 10.2475/06.2016.02] COSMOGENIC-NUCLIDE EXPOSURE AGES FROM THE PENSACOLA MOUNTAINS ADJACENT TO THE FOUNDATION ICE STREAM, ANTARCTICA GREG BALCO*,†, CLAIRE TODD**, KATHLEEN HUYBERS***, SETH CAMPBELL§, MICHAEL VERMEULEN**, MATTHEW HEGLAND**, BRENT M. GOEHRING§§, AND TREVOR R. HILLEBRAND*** ABSTRACT. We describe glacial-geological observations and cosmogenic-nuclide exposure ages from the Schmidt, Williams, and Thomas Hills in the Pensacola Mountains of Antarctica adjacent to the Foundation Ice Stream (FIS). Our aim is to learn about changes in the thickness and grounding line position of the Antarctic Ice Sheet in the Weddell Sea embayment between the Last Glacial Maximum (LGM) and the present. Glacial-geological observations from all three regions indicate that currently- ice-free areas were covered by ice during one or more past ice sheet expansions, and that this ice was typically frozen to its bed and thus non-erosive, permitting the accumulation of multiple generations of glacial drift. Cosmogenic-nuclide exposure- age data from glacially transported erratics are consistent with this interpretation in that we observe both (i) samples with Holocene exposure ages that display a systematic age-elevation relationship recording LGM-to-present deglaciation, and (ii) samples with older and highly scattered apparent exposure ages that were deposited in previous glacial-interglacial cycles and have experienced multiple periods of surface exposure and ice cover. Holocene exposure ages at the Thomas and Williams Hills, upstream of the present grounding line of the FIS, show that the FIS was at least 500 m thicker prior to 11 ka, and that 500 m of thinning took place between 11 and 4 ka. -
Terrestrial Geology and Geophysics
Terrestrial geology and geophysics Uplift of the shoulder escarpment rift system and the rift shoulder. If a maximum uplift of 5-6 kilometers in the southern Victoria Land or 10 kilometers in of the west antarctic northern Victoria Land (Fitzgerald 1989) area is correct, then rift system and its relation 1-2 kilometers and as much as 6 kilometers, respectively, of erosion has occurred from the highest topography in these two to Late Cenozoic climate change areas to result in the maximum altitude of about 4 kilometers observed now. The variation of the high topography seen in figure 2 along the rift shoulder is probably caused by erosion JOHN C. BEHRENDT and differential uplift (Behrendt and Cooper in press). We interpret that the main cause of uplift, along the west antarctic U.S. Geological Survei rift shoulder, is late Cenozoic tectonism associated with rifting, Denver Federal Center probably as modeled by Stern and ten Brink (1989), for a con- Denver, Colorado 80225 tinental lithospheric plate heated at the free edge. The maximum elevations (figure 2) vary from about 4 kilo- meters in Victoria Land and the Queen Maud Mountains (fig- ALAN COOPER ure 1), dropping to about 3 kilometers in the Horlick and Whitmore mountains (perhaps resulting from a greater rate of U.S. Geological Survey erosion) and rising again to 5 kilometers in the Ellsworth Menlo Park, California 94025 Mountains. In contrast, elevations along the Transantarctic Mountains are much lower toward the Weddell Sea (see the The Cenozoic West Antarctic rift system (Behrendt and Cooper solid-line profile of figure 2). -
US Geological Survey Scientific Activities in the Exploration of Antarctica: 1946–2006 Record of Personnel in Antarctica and Their Postal Cachets: US Navy (1946–48, 1954–60), International
Prepared in cooperation with United States Antarctic Program, National Science Foundation U.S. Geological Survey Scientific Activities in the Exploration of Antarctica: 1946–2006 Record of Personnel in Antarctica and their Postal Cachets: U.S. Navy (1946–48, 1954–60), International Geophysical Year (1957–58), and USGS (1960–2006) By Tony K. Meunier Richard S. Williams, Jr., and Jane G. Ferrigno, Editors Open-File Report 2006–1116 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior DIRK KEMPTHORNE, Secretary U.S. Geological Survey Mark D. Myers, Director U.S. Geological Survey, Reston, Virginia 2007 For product and ordering information: World Wide Web: http://www.usgs.gov/pubprod Telephone: 1-888-ASK-USGS For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment: World Wide Web: http://www.usgs.gov Telephone: 1-888-ASK-USGS Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted material contained within this report. Cover: 2006 postal cachet commemorating sixty years of USGS scientific innovation in Antarctica (designed by Kenneth W. Murphy and Tony K. Meunier, art work by Kenneth W. Murphy). ii Table of Contents Introduction......................................................................................................................................................................1 Selected.References.........................................................................................................................................................2