Workshop on Antarctic Glaciology and Meteorites
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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. -
Isotopic Oxygen-18 Results from Blue-Ice Areas
Isotopic oxygen-18 results Tongue blue-ice field ranges in 8180 from –40.7 to –58.8 parts per thousand. In a 200-meter transect with a sample every 10 from blue-ice areas meters, a 60-meter area of "yellow" or "dirty" ice has an av- erage 8180 value of –42.8 ± 1.4 parts per thousand, while the average for the blue-ice is –54.4 ± 0.3 parts per thousand. P.M. GROOTES and M. STUIVER Lighter 8110 values seem also to be associated with the me- teorite-carrying ice. Detailed sampling on five large sample Quaternary Isotope Laboratory blocks showed no signs of sample contamination and enrich- University of Washington ment. Seattle, Washington 98195 The observed i8O range is more than triple the glacial/in- terglacial 8180 change and the isotopically light ice, therefore, We measured the oxygen isotope abundance ratio oxygen - must have originated in the high interior of East Antarctica. 18/oxygen-16 in three sets of samples from blue-ice ablation The most negative value of –58.8 parts per thousand is, how- areas west of the Transantarctic Mountains. Samples were col- ever, still lighter than present snow accumulating at the Pole lected at the Reckling Moraine (by C. Faure), the Lewis Cliff of Relative Inaccessibility (-57 parts per thousand, Lorius 1983). Ice Tongue (by W.A. Cassidy, submitted by P. Englert), and If this ice had been formed during a glacial period, the source the Allan Hills (by J.O. Annexstad). Most samples were cut area could be closer to the Transantarctic Mountains. -
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. -
Glacier Lake, Saddle, & Blue Ice Trails
Guide to Glacier Lake, Saddle, & Blue Ice Trails in Kachemak Bay State Park Trail Access: Glacier Spit, Saddle, or Humpy Creek Grewingk Tram Spur (1 mile, easy) Allowable Uses: Hiking This spur connects Glacier Distance: 3.2 mi one-way (Glacier Lake Trail) Lake Trail and Emerald Lake Loop Trail. There is a hand- 1.0 mi one way (Saddle Trail) operated cable car pulley 6.7 mi one-way (Glacier Spit to Blue Ice Trail end) system over Grewingk Elevation Gain: 200 ft (Glacier Lake Trail) Creek. Operation requires 200 ft (Glacier Lake to Saddle Trailhead) two people. Maximum capacity of the tram is 500 500 ft (Glacier Spit to Blue Ice Trail end) pounds. If only two people are crossing the Difficulty: Easy; family suitable (Glacier Lake Trail) tram, one person should stay behind and assist in Camping: Moderate (Saddle Trail) pulling the other across. Two people in the tram cart without assistance from others on the plat- Glacier Spit, Grewingk Glacier Lake, Grewingk Creek, Moderate (Blue Ice Trail) form is difficult. Gloves are helpful in operating Tarn Lake, Humpy Creek, Right Beach (accessible at Hiking Time: 1.5 hours (to end Glacier Lake Trail) low tide from Glacier Spit) the tram. 30 minutes (Saddle Trail) Water Availability: 5 hours (Glacier Spit to Blue Ice Trail end) Glacier Lake & Saddle Trails: Grewingk Creek (glacial), Grewingk Glacier Lake A Popular route joins the Saddle and Glacier Lake (glacial), small streams near glacier and on Saddle Tr. Blue Ice Trail: Trails. The Glacier Lake Trail follows flat terrain Safety and Considerations: This is the only developed access to Grewingk through stands of cottonwoods & spruce, and CAUTION: Unless properly trained and outfitted for Glacier. -
Antarctic Surface and Subsurface Snow and Ice Melt Fluxes
15 MAY 2005 L I S T O N A N D W I N THER 1469 Antarctic Surface and Subsurface Snow and Ice Melt Fluxes GLEN E. LISTON Department of Atmospheric Science, Colorado State University, Fort Collins, Colorado JAN-GUNNAR WINTHER Norwegian Polar Institute, Polar Environmental Centre, Tromsø, Norway (Manuscript received 19 April 2004, in final form 22 October 2004) ABSTRACT This paper presents modeled surface and subsurface melt fluxes across near-coastal Antarctica. Simula- tions were performed using a physical-based energy balance model developed in conjunction with detailed field measurements in a mixed snow and blue-ice area of Dronning Maud Land, Antarctica. The model was combined with a satellite-derived map of Antarctic snow and blue-ice areas, 10 yr (1991–2000) of Antarctic meteorological station data, and a high-resolution meteorological distribution model, to provide daily simulated melt values on a 1-km grid covering Antarctica. Model simulations showed that 11.8% and 21.6% of the Antarctic continent experienced surface and subsurface melt, respectively. In addition, the simula- tions produced 10-yr averaged subsurface meltwater production fluxes of 316.5 and 57.4 km3 yrϪ1 for snow-covered and blue-ice areas, respectively. The corresponding figures for surface melt were 46.0 and 2.0 km3 yrϪ1, respectively, thus demonstrating the dominant role of subsurface over surface meltwater pro- duction. In total, computed surface and subsurface meltwater production values equal 31 mm yrϪ1 if evenly distributed over all of Antarctica. While, at any given location, meltwater production rates were highest in blue-ice areas, total annual Antarctic meltwater production was highest for snow-covered areas due to its larger spatial extent. -
Glacier Mass Balance This Summary Follows the Terminology Proposed by Cogley Et Al
Summer school in Glaciology, McCarthy 5-15 June 2018 Regine Hock Geophysical Institute, University of Alaska, Fairbanks Glacier Mass Balance This summary follows the terminology proposed by Cogley et al. (2011) 1. Introduction: Definitions and processes Definition: Mass balance is the change in the mass of a glacier, or part of the glacier, over a stated span of time: t . ΔM = ∫ Mdt t1 The term mass budget is a synonym. The span of time is often a year or a season. A seasonal mass balance is nearly always either a winter balance or a summer balance, although other kinds of seasons are appropriate in some climates, such as those of the tropics. The definition of “year” depends on the measurement method€ (see Chap. 4). The mass balance, b, is the sum of accumulation, c, and ablation, a (the ablation is defined here as negative). The symbol, b (for point balances) and B (for glacier-wide balances) has traditionally been used in studies of surface mass balance of valley glaciers. t . b = c + a = ∫ (c+ a)dt t1 Mass balance is often treated as a rate, b dot or B dot. Accumulation Definition: € 1. All processes that add to the mass of the glacier. 2. The mass gained by the operation of any of the processes of sense 1, expressed as a positive number. Components: • Snow fall (usually the most important). • Deposition of hoar (a layer of ice crystals, usually cup-shaped and facetted, formed by vapour transfer (sublimation followed by deposition) within dry snow beneath the snow surface), freezing rain, solid precipitation in forms other than snow (re-sublimation composes 5-10% of the accumulation on Ross Ice Shelf, Antarctica). -
Build-Up and Chronology of Blue Ice Moraines in Queen Maud Land, Antarctica
Research Collection Journal Article Build-up and chronology of blue ice moraines in Queen Maud Land, Antarctica Author(s): Akçar, Naki; Yeşilyurt, Serdar; Hippe, Kristina; Christl, Marcus; Vockenhuber, Christof; Yavuz, Vural; Özsoy, Burcu Publication Date: 2020-10 Permanent Link: https://doi.org/10.3929/ethz-b-000444919 Originally published in: Quaternary Science Advances 2, http://doi.org/10.1016/j.qsa.2020.100012 Rights / License: Creative Commons Attribution 4.0 International This page was generated automatically upon download from the ETH Zurich Research Collection. For more information please consult the Terms of use. ETH Library Quaternary Science Advances 2 (2020) 100012 Contents lists available at ScienceDirect Quaternary Science Advances journal homepage: www.journals.elsevier.com/quaternary-science-advances Build-up and chronology of blue ice moraines in Queen Maud Land, Antarctica Naki Akçar a,b,*, Serdar Yes¸ilyurt a,c, Kristina Hippe d, Marcus Christl d, Christof Vockenhuber d, Vural Yavuz e, Burcu Ozsoy€ b,f a Institute of Geological Sciences, University of Bern, Baltzerstrasse 1-3, 3012, Bern, Switzerland b Polar Research Institute, TÜBITAK Marmara Research Center, Gebze, Istanbul, Turkey c Department of Geography, Ankara University, Sıhhiye, 06100, Ankara, Turkey d Laboratory of Ion Beam Physics (LIP), ETH Zurich, Otto-Stern-Weg 5, 8093, Zurich, Switzerland e Faculty of Engineering, Turkish-German University, 34820, Beykoz, Istanbul, Turkey f Maritime Faculty, Istanbul Technical University Tuzla Campus, Istanbul, Turkey -
Navigating Troubled Waters a History of Commercial Fishing in Glacier Bay, Alaska
National Park Service U.S. Department of the Interior Glacier Bay National Park and Preserve Navigating Troubled Waters A History of Commercial Fishing in Glacier Bay, Alaska Author: James Mackovjak National Park Service U.S. Department of the Interior Glacier Bay National Park and Preserve “If people want both to preserve the sea and extract the full benefit from it, they must now moderate their demands and structure them. They must put aside ideas of the sea’s immensity and power, and instead take stewardship of the ocean, with all the privileges and responsibilities that implies.” —The Economist, 1998 Navigating Troubled Waters: Part 1: A History of Commercial Fishing in Glacier Bay, Alaska Part 2: Hoonah’s “Million Dollar Fleet” U.S. Department of the Interior National Park Service Glacier Bay National Park and Preserve Gustavus, Alaska Author: James Mackovjak 2010 Front cover: Duke Rothwell’s Dungeness crab vessel Adeline in Bartlett Cove, ca. 1970 (courtesy Charles V. Yanda) Back cover: Detail, Bartlett Cove waters, ca. 1970 (courtesy Charles V. Yanda) Dedication This book is dedicated to Bob Howe, who was superintendent of Glacier Bay National Monument from 1966 until 1975 and a great friend of the author. Bob’s enthusiasm for Glacier Bay and Alaska were an inspiration to all who had the good fortune to know him. Part 1: A History of Commercial Fishing in Glacier Bay, Alaska Table of Contents List of Tables vi Preface vii Foreword ix Author’s Note xi Stylistic Notes and Other Details xii Chapter 1: Early Fishing and Fish Processing in Glacier Bay 1 Physical Setting 1 Native Fishing 1 The Coming of Industrial Fishing: Sockeye Salmon Attract Salters and Cannerymen to Glacier Bay 4 Unnamed Saltery at Bartlett Cove 4 Bartlett Bay Packing Co. -
The Dominion Range Ice Core, Queen Maud Mountains, Antarctica - General Site and Core Characteristics with Implications
University of New Hampshire University of New Hampshire Scholars' Repository Faculty Publications 1-20-2017 The Dominion Range Ice Core, Queen Maud Mountains, Antarctica - General Site and Core Characteristics with Implications Paul A. Mayewski University of Maine Mark S. Twickler University of New Hampshire, Durham, [email protected] W. Berry Lyons University of New Hampshire, Durham Mary Jo Spencer University of New Hampshire, Durham Debra A. Meese U.S. Army Cold Regions Research and Engineering Laboratory See next page for additional authors Follow this and additional works at: https://scholars.unh.edu/faculty_pubs Recommended Citation Mayewski, P. A., Twickler, M. S., Lyons, W. B., Spencer, M. J., Meese, D. A., Gow, A. J., . Saltzman, E. (1990). The Dominion Range Ice Core, Queen Maud Mountains, Antarctica - General Site and Core Characteristics with Implications. Journal of Glaciology, 36(122), 11-16. doi:10.1017/ S0022143000005499 This Article is brought to you for free and open access by University of New Hampshire Scholars' Repository. It has been accepted for inclusion in Faculty Publications by an authorized administrator of University of New Hampshire Scholars' Repository. For more information, please contact [email protected]. Authors Paul A. Mayewski, Mark S. Twickler, W. Berry Lyons, Mary Jo Spencer, Debra A. Meese, Anthony J. Gow, Pieter M. Grootes, Todd Sowers, M. Scott Watson, and Eric Saltzman This article is available at University of New Hampshire Scholars' Repository: https://scholars.unh.edu/faculty_pubs/ 375 loumal oJ Glaciology, Vol. 36, No. 122, 1990 THE DOMINION RANGE ICE CORE, QUEEN MAUD MOUNTAINS, ANTARCTICA - GENERAL SITE AND CORE CHARACTERISTICS WITH IMPLICATIONS By PAUL A. -
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. -
1 Compiled by Mike Wing New Zealand Antarctic Society (Inc
ANTARCTIC 1 Compiled by Mike Wing US bulldozer, 1: 202, 340, 12: 54, New Zealand Antarctic Society (Inc) ACECRC, see Antarctic Climate & Ecosystems Cooperation Research Centre Volume 1-26: June 2009 Acevedo, Capitan. A.O. 4: 36, Ackerman, Piers, 21: 16, Vessel names are shown viz: “Aconcagua” Ackroyd, Lieut. F: 1: 307, All book reviews are shown under ‘Book Reviews’ Ackroyd-Kelly, J. W., 10: 279, All Universities are shown under ‘Universities’ “Aconcagua”, 1: 261 Aircraft types appear under Aircraft. Acta Palaeontolegica Polonica, 25: 64, Obituaries & Tributes are shown under 'Obituaries', ACZP, see Antarctic Convergence Zone Project see also individual names. Adam, Dieter, 13: 6, 287, Adam, Dr James, 1: 227, 241, 280, Vol 20 page numbers 27-36 are shared by both Adams, Chris, 11: 198, 274, 12: 331, 396, double issues 1&2 and 3&4. Those in double issue Adams, Dieter, 12: 294, 3&4 are marked accordingly. Adams, Ian, 1: 71, 99, 167, 229, 263, 330, 2: 23, Adams, J.B., 26: 22, Adams, Lt. R.D., 2: 127, 159, 208, Adams, Sir Jameson Obituary, 3: 76, A Adams Cape, 1: 248, Adams Glacier, 2: 425, Adams Island, 4: 201, 302, “101 In Sung”, f/v, 21: 36, Adamson, R.G. 3: 474-45, 4: 6, 62, 116, 166, 224, ‘A’ Hut restorations, 12: 175, 220, 25: 16, 277, Aaron, Edwin, 11: 55, Adare, Cape - see Hallett Station Abbiss, Jane, 20: 8, Addison, Vicki, 24: 33, Aboa Station, (Finland) 12: 227, 13: 114, Adelaide Island (Base T), see Bases F.I.D.S. Abbott, Dr N.D. -
Glaciers: Clues to Future Climate?
Glaciers: Clues to Future Climate? Glaciers: Clues to Future Climate? by Richard S. Williams, Jr. Cover photograph: The ship Island Princess and the calving terminus of Johns Hopkins Glacier, Glacier Bay National Monument, Alaska (oblique aerial photo by Austin Post, Sept. 2, 1977) Oblique aerial photo of valley glaciers in Mt. McKinley National Park, Alaska (photo by Richard S. Williams, Jr., Oct. 4, 1965) Vertical aerial photo of severely crevassed glaciers on the slopes of Cotopaxi, a nearly sym- metrical volcano, near the Equator in north-central Equador (photo courtesy of U.S. Air Force). A glacier is a large mass of ice having its genesis on land and repre- sents a multiyear surplus of snowfall over snowmelt. At the present time, perennial ice covers about 10 percent of the land areas of the Earth. Although glaciers are generally thought of as polar entities, they also are found in mountainous areas throughout the world, on all continents except Australia, and even at or near the Equator on high mountains in Africa and South America. 2 Streamflow from the terminus of the Mammoth Glacier, Wind River Range, Montana (photo by Mark F. Meier, August 1950). Present-day glaciers and the deposits from more extensive glaciation in the geological past have considerable economic importance in many areas. In areas of limited precipitation during the growing season, for example, such as parts of the Western United States, glaciers are consid- ered to be frozen freshwater reservoirs which release water during the drier summer months. In the Western United States, as in many other mountainous regions, they are of considerable economic importance in the irrigation of crops and to the generation of hydroelectric power.