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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. -
The Commonwealth Trans-Antarctic Expedition 1955-1958
THE COMMONWEALTH TRANS-ANTARCTIC EXPEDITION 1955-1958 HOW THE CROSSING OF ANTARCTICA MOVED NEW ZEALAND TO RECOGNISE ITS ANTARCTIC HERITAGE AND TAKE AN EQUAL PLACE AMONG ANTARCTIC NATIONS A thesis submitted in fulfilment of the requirements for the Degree PhD - Doctor of Philosophy (Antarctic Studies – History) University of Canterbury Gateway Antarctica Stephen Walter Hicks 2015 Statement of Authority & Originality I certify that the work in this thesis has not been previously submitted for a degree nor has it been submitted as part of requirements for a degree except as fully acknowledged within the text. I also certify that the thesis has been written by me. Any help that I have received in my research and the preparation of the thesis itself has been acknowledged. In addition, I certify that all information sources and literature used are indicated in the thesis. Elements of material covered in Chapter 4 and 5 have been published in: Electronic version: Stephen Hicks, Bryan Storey, Philippa Mein-Smith, ‘Against All Odds: the birth of the Commonwealth Trans-Antarctic Expedition, 1955-1958’, Polar Record, Volume00,(0), pp.1-12, (2011), Cambridge University Press, 2011. Print version: Stephen Hicks, Bryan Storey, Philippa Mein-Smith, ‘Against All Odds: the birth of the Commonwealth Trans-Antarctic Expedition, 1955-1958’, Polar Record, Volume 49, Issue 1, pp. 50-61, Cambridge University Press, 2013 Signature of Candidate ________________________________ Table of Contents Foreword .................................................................................................................................. -
The Antarctic Sun, December 28, 2003
Published during the austral summer at McMurdo Station, Antarctica, for the United States Antarctic Program December 28, 2003 Photo by Kristan Hutchison / The Antarctic Sun A helicopter lands behind the kitchen and communications tents at Beardmore Camp in mid-December. Back to Beardmore: By Kristan Hutchison Researchers explore the past from temporary camp Sun staff ike the mythical town of Brigadoon, a village of tents appears on a glacial arm 50 miles L from Beardmore Glacier about once a decade, then disappears. It, too, is a place lost in time. For most people, a visit to Beardmore Camp is a trip back in history, whether to the original camp structure from 19 years ago, now buried under snow, or to the sites of ancient forests and bones, now buried under rock. Ever since Robert Scott collected fos- sils on his way back down the Beardmore Glacier in February 1912, geologists and paleontologists have had an interest in the rocky outcrops lining the broad river of ice. This year’s Beardmore Camp was the third at the location on the Lennox-King Glacier and the researchers left, saying there Photo by Andy Sajor / Special to The Antarctic Sun Researchers cut dinosaur bones out of the exposed stone on Mt. Kirkpatrick in December. See Camp on page 7 Some of the bones are expected to be from a previously unknown type. INSIDE Quote of the Week Dinosaur hunters Fishing for fossils “The penguins are happier than Page 9 Page 11 Trackers clams.” Plant gatherers - Adelie penguin researcher summing Page 10 Page 12 up the attitude of a colony www.polar.org/antsun 2 • The Antarctic Sun December 28, 2003 Ross Island Chronicles By Chico That’s the way it is with time son. -
Bulletin Vol. 13 No. 1 ANTARCTIC PENINSULA O 1 0 0 K M Q I Q O M L S
ANttlcnc Bulletin Vol. 13 No. 1 ANTARCTIC PENINSULA O 1 0 0 k m Q I Q O m l s 1 Comandante fettai brazil 2 Henry Arctowski poono 3 Teniente Jubany Argentina 4 Artigas Uruguay 5 Teniente Rodolfo Marsh chile Bellingshausen ussr Great Wall china 6 Capitan Arturo Prat chile 7 General Bernardo O'Higgins chile 8 Esperania argentine 9 Vice Comodoro Marambio Argentina 10 Palmer us* 11 Faraday uk SOUTH 12 Rotheraux 13 Teniente Carvajal chile SHETLAND 14 General San Martin Argentina ISLANDS jOOkm NEW ZEALAND ANTARCTIC SOCIETY MAP COPYRIGHT Vol.l3.No.l March 1993 Antarctic Antarctic (successor to the "Antarctic News Bulletin") Vol. 13 No. 1 Issue No. 145 ^H2£^v March.. 1993. .ooo Contents Polar New Zealand 2 Australia 9 ANTARCTIC is published Chile 15 quarterly by the New Zealand Antarctic Italy 16 Society Inc., 1979 United Kingdom 20 United States 20 ISSN 0003-5327 Sub-antarctic Editor: Robin Ormerod Please address all editorial inquiries, Heard and McDonald 11 contributions etc to the Macquarie and Campbell 22 Editor, P.O. Box 2110, Wellington, New Zealand General Telephone: (04) 4791.226 CCAMLR 23 International: +64 + 4+ 4791.226 Fax: (04) 4791.185 Whale sanctuary 26 International: +64 + 4 + 4791.185 Greenpeace 28 First footings at Pole 30 All administrative inquiries should go to Feinnes and Stroud, Kagge the Secretary, P.O. Box 2110, Wellington and the Women's team New Zealand. Ice biking 35 Inquiries regarding back issues should go Vaughan expedition 36 to P.O. Box 404, Christchurch, New Zealand. Cover: Ice biking: Trevor Chinn contem plates biking the glacier slope to the Polar (S) No part of this publication may be Plateau, Mt. -
Ernest Shackleton and the Epic Voyage of the Endurance
9-803-127 REV: DECEMBER 2, 2010 NANCY F. KOEHN Leadership in Crisis: Ernest Shackleton and the Epic Voyage of the Endurance For scientific discovery give me Scott; for speed and efficiency of travel give me Amundsen; but when disaster strikes and all hope is gone, get down on your knees and pray for Shackleton. — Sir Raymond Priestley, Antarctic Explorer and Geologist On January 18, 1915, the ship Endurance, carrying a highly celebrated British polar expedition, froze into the icy waters off the coast of Antarctica. The leader of the expedition, Sir Ernest Shackleton, had planned to sail his boat to the coast through the Weddell Sea, which bounded Antarctica to the north, and then march a crew of six men, supported by dogs and sledges, to the Ross Sea on the opposite side of the continent (see Exhibit 1).1 Deep in the southern hemisphere, it was early in the summer, and the Endurance was within sight of land, so Shackleton still had reason to anticipate reaching shore. The ice, however, was unusually thick for the ship’s latitude, and an unexpected southern wind froze it solid around the ship. Within hours the Endurance was completely beset, a wooden island in a sea of ice. More than eight months later, the ice still held the vessel. Instead of melting and allowing the crew to proceed on its mission, the ice, moving with ocean currents, had carried the boat over 670 miles north.2 As it moved, the ice slowly began to soften, and the tremendous force of distant currents alternately broke apart the floes—wide plateaus made of thousands of tons of ice—and pressed them back together, creating rift lines with huge piles of broken ice slabs. -
2010-2011 Science Planning Summaries
Find information about current Link to project web sites and USAP projects using the find information about the principal investigator, event research and people involved. number station, and other indexes. Science Program Indexes: 2010-2011 Find information about current USAP projects using the Project Web Sites principal investigator, event number station, and other Principal Investigator Index indexes. USAP Program Indexes Aeronomy and Astrophysics Dr. Vladimir Papitashvili, program manager Organisms and Ecosystems Find more information about USAP projects by viewing Dr. Roberta Marinelli, program manager individual project web sites. Earth Sciences Dr. Alexandra Isern, program manager Glaciology 2010-2011 Field Season Dr. Julie Palais, program manager Other Information: Ocean and Atmospheric Sciences Dr. Peter Milne, program manager Home Page Artists and Writers Peter West, program manager Station Schedules International Polar Year (IPY) Education and Outreach Air Operations Renee D. Crain, program manager Valentine Kass, program manager Staffed Field Camps Sandra Welch, program manager Event Numbering System Integrated System Science Dr. Lisa Clough, program manager Institution Index USAP Station and Ship Indexes Amundsen-Scott South Pole Station McMurdo Station Palmer Station RVIB Nathaniel B. Palmer ARSV Laurence M. Gould Special Projects ODEN Icebreaker Event Number Index Technical Event Index Deploying Team Members Index Project Web Sites: 2010-2011 Find information about current USAP projects using the Principal Investigator Event No. Project Title principal investigator, event number station, and other indexes. Ainley, David B-031-M Adelie Penguin response to climate change at the individual, colony and metapopulation levels Amsler, Charles B-022-P Collaborative Research: The Find more information about chemical ecology of shallow- USAP projects by viewing individual project web sites. -
2003-2004 Science Planning Summary
2003-2004 USAP Field Season Table of Contents Project Indexes Project Websites Station Schedules Technical Events Environmental and Health & Safety Initiatives 2003-2004 USAP Field Season Table of Contents Project Indexes Project Websites Station Schedules Technical Events Environmental and Health & Safety Initiatives 2003-2004 USAP Field Season Project Indexes Project websites List of projects by principal investigator List of projects by USAP program List of projects by institution List of projects by station List of projects by event number digits List of deploying team members Teachers Experiencing Antarctica Scouting In Antarctica Technical Events Media Visitors 2003-2004 USAP Field Season USAP Station Schedules Click on the station name below to retrieve a list of projects supported by that station. Austral Summer Season Austral Estimated Population Openings Winter Season Station Operational Science Opening Summer Winter 20 August 01 September 890 (weekly 23 February 187 McMurdo 2003 2003 average) 2004 (winter total) (WinFly*) (mainbody) 2,900 (total) 232 (weekly South 24 October 30 October 15 February 72 average) Pole 2003 2003 2004 (winter total) 650 (total) 27- 34-44 (weekly 17 October 40 Palmer September- 8 April 2004 average) 2003 (winter total) 2003 75 (total) Year-round operations RV/IB NBP RV LMG Research 39 science & 32 science & staff Vessels Vessel schedules on the Internet: staff 25 crew http://www.polar.org/science/marine. 25 crew Field Camps Air Support * A limited number of science projects deploy at WinFly. 2003-2004 USAP Field Season Technical Events Every field season, the USAP sponsors a variety of technical events that are not scientific research projects but support one or more science projects. -
Antarctic Connections: Christchurch & Canterbury
Antarctic Connections: Christchurch & Canterbury Morning, Discovery and Terra Nova at the Port of Lyttelton following the British Antarctic (Discovery) Expedition, 1904. (http://www.nzhistory.net.nz/media/photo/captain-scotts-ships-lyttelton) A guide to the past and present connections of Antarctica to Christchurch and the greater Canterbury region. 1 Compiled by James Stone, 2015. Cover 1 Contents 2 Christchurch – Gateway to the Antarctic 3 Significant Events in Canterbury’s Antarctic History 4 The Early Navigators 5 • Captain James Cook • Sir Joseph Banks • Sealers & Whalers Explorers of the Heroic Age • Captain Robert Falcon Scott 6-9 • Dr Edward Wilson 10-11 • Uncle Bill’s Cabin • Herbert Ponting 12 • Roald Amundsen 13-14 • Sir Ernest Shackleton 15-18 • Frank Arthur Worsley 19 • The Ross Sea Party 20-21 • Sir Douglas Mawson 22 The IGY and the Scientific Age 22 Operation Deep Freeze 23-24 First Māori Connection 25 The IGY and the Scientific Age 26 Hillary’s Trans-Antarctic Expedition (TAE) 27 NZ Antarctic Heritage Trust 28 • Levick’s Notebook 28 • Ross Sea Lost Photographs 29 • Shackleton’s Whisky 30 • NZ Antarctic Society 31 Scott Base 32 International Collaboration 33 • Antarctic Campus • Antarctica New Zealand • United States Antarctic Program • Italian Antarctic Program 34 • Korean Antarctic Program Tourism 35 The Erebus Disaster 36 Antarctic Connections by location • Christchurch (Walking tour map 47) 37-47 • Lyttelton (Walking tour map 56) 48-56 • Quail Island 57-59 • Akaroa (Walking tour map 61) 60-61 Visiting Antarctic Wildlife 62 Attractions by Explorer 63 Business Links 64-65 Contact 65 Useful Links 66-69 2 Christchurch – Gateway to the Antarctic nzhistory.net.nz © J Stone © J Stone Christchurch has a long history of involvement with the Antarctic, from the early days of Southern Ocean exploration, as a vital port during the heroic era expeditions of discovery and the scientific age of the International Geophysical Year, through to today as a hub of Antarctic research and logistics. -
Holocene Thinning of Darwin and Hatherton Glaciers, Antarctica, and Implications for Grounding-Line Retreat in the Ross Sea
The Cryosphere, 15, 3329–3354, 2021 https://doi.org/10.5194/tc-15-3329-2021 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. Holocene thinning of Darwin and Hatherton glaciers, Antarctica, and implications for grounding-line retreat in the Ross Sea Trevor R. Hillebrand1,a, John O. Stone1, Michelle Koutnik1, Courtney King2, Howard Conway1, Brenda Hall2, Keir Nichols3, Brent Goehring3, and Mette K. Gillespie4 1Department of Earth and Space Sciences, University of Washington, Seattle, WA 98195, USA 2School of Earth and Climate Science and Climate Change Institute, University of Maine, Orono, ME 04469, USA 3Department of Earth and Environmental Sciences, Tulane University, New Orleans, LA 70118, USA 4Faculty of Engineering and Science, Western Norway University of Applied Sciences, Sogndal, 6856, Norway anow at: Fluid Dynamics and Solid Mechanics Group, Los Alamos National Laboratory, Los Alamos, NM 87545, USA Correspondence: Trevor R. Hillebrand ([email protected]) Received: 8 December 2020 – Discussion started: 15 December 2020 Revised: 4 May 2021 – Accepted: 27 May 2021 – Published: 20 July 2021 Abstract. Chronologies of glacier deposits in the available records from the mouths of other outlet glaciers Transantarctic Mountains provide important constraints in the Transantarctic Mountains, many of which thinned by on grounding-line retreat during the last deglaciation in hundreds of meters over roughly a 1000-year period in the the Ross Sea. However, between Beardmore Glacier and Early Holocene. The deglaciation histories of Darwin and Ross Island – a distance of some 600 km – the existing Hatherton glaciers are best matched by a steady decrease in chronologies are generally sparse and far from the modern catchment area through the Holocene, suggesting that Byrd grounding line, leaving the past dynamics of this vast region and/or Mulock glaciers may have captured roughly half of largely unconstrained. -
Antarctic Glacial Chronology: New Constraints from Surface Exposure Dating
Antarctic Glacial Chronology: New constraints from surface exposure dating by Robert P. Ackert Jr. B.A., University ofMaine, 1979 M.S., University ofMaine, 1990 Submitted in partial fulfillment ofthe requirements for the degree of DOCTOR OF PHILOSOPHY at the MASSACHUSETTS INSTITUTE OF TECHNOLOGY and the WOODS HOLE OCEANOGRAPHIC INSTITUTION JUNE 2000 © 2000 Robert P. Ackert Jr. all rights reserved The author hereby grants to MIT and WHOI pennission to reproduce paper and electronic copies ofthis thesis in whole or in part, and to distribute them publicly. Signature ofAuthor__~~~~_L...-----L(""""'_.~('r-=:::;;£....JI./(;.....::,::racy~::......-----&~ _ Joint Program in Oceanography Massachusetts Institute ofTechnology And Woods Hole Oceanographic Institution May 5, 2000 Certified Dr. Mark D. Kurz Thesis Supervisor Accepted by --=-- ...L-, _ Dr. Timohty L. Grove Chaihnan, Joint Committee for Marine Geology and Geophysics Massachusetts Institute ofTechnology / Woods Hole Oceanographic Institution Antarctic Glacial Chronology: New constraints from surface exposure dating by Robert P. Ackert Jr. Submitted to the Massachusetts Institute ofTechnology Woods Hole Oceanographic Institution Joint Program in Oceanography on May 5, 2000, in partial fulfillment ofthe requirements for the degree of Doctor ofPhilosophy Abstract Surface exposure dating, using the concentration ofcosmogenic nuclides c'He, 21 Ne, and 36Cl) in moraine boulders, combined with mapping ofglacial moraines from three key locations, is used to provide new constraints to Antarctic glacial chronology. The results are used to reconstruct past West Antarctic Ice Sheet (WAIS) geometry and test models ofWAIS behavior. Mount Waesche is a volcanic nunatak near the dome ofthe WAIS in Marie Byrd Land. The Dominion Range is at the head ofthe Beardmore Glacier, an outlet glacier of the East Antarctic Ice Sheet in the Transantarctic Mountains. -
First Evidence of a Tetrapod Footprint from the Triassic of Northern Victoria Land, Antarctica
RESEARCH NOTE First evidence of a tetrapod footprint from the Triassic of northern Victoria Land, Antarctica Thomas Mörs1, Grzegorz Niedz´wiedzki2, Laura Crispini3, Andreas Läufer4 & Benjamin Bomfleur5 1 Department of Palaeobiology, Swedish Museum of Natural History, Stockholm, Sweden; 2 Subdepartment of Evolution and Development, Department of Organismal Biology, Uppsala University, Uppsala, Sweden 3 Dipartimento di Scienze della Terra, Ambiente e Vita, University of Genova, Genoa, Italy; 4 Federal Institute for Geosciences and Natural Resources (BGR), Hannover, Germany; 5 Palaeobotany Research Group, Institut für Geologie und Paläontologie, Westfälische Wilhelms-Universität Münster, Münster, Germany Abstract Keywords Beacon Supergroup; Helliwell Hills; Here, we report on a tetrapod footprint from the Transantarctic Basin in the far ichnotaxon; Procolophonichnium; Rennick north of Victoria Land, which marks the first record of terrestrial vertebrates for Glacier; Transantarctic Basin this region. The single specimen derives from a previously unknown lithologi- cal unit of Middle or Late Triassic age of the Beacon Supergroup in the Helliwell Correspondence Hills in the central Rennick Glacier area. It differs in both size and morphology Thomas Mörs, Department of Palaeobiology, clearly from Middle Triassic trackway types from the upper Fremouw Forma- Swedish Museum of Natural History, tion of the Queen Alexandra Range in southern Victoria Land, and likely rep- P.O. Box 50007, SE-104 05 Stockholm, Sweden. E-mail: [email protected] resents a primitive amniote, procolophonid or therapsid. The footprint is the third evidence of fossil vertebrate trackways in Antarctica. Introduction been discovered in the upper Fremouw Formation of the Queen Alexandra Range (Macdonald et al. 1991). Since the first terrestrial tetrapod fossil was described Together with avian tracks from the Eocene Fossil Hill from the central Transantarctic Mountains in Antarc- Formation at Fildes Peninsula on King George Island, tica (Barrett et al. -
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