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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. -
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. -
University Microfilms, a XEROX Company, Ann Arbor, Michigan
I I 72-4508 GUNNER, John Duncan, 1945- AGE AND ORIGIN OF THE NIMROD GROUP AND OF THE GRANITE HARBOUR INTRUSIVES, BEARDMORE GLACIER REGION, ANTARCTICA. The Ohio State University, Ph.D., 1971 Geology University Microfilms, A XEROX Company, Ann Arbor, Michigan THIS DISSERTATION HAS BEEN MICROFILMED EXACTLY AS RECEIVED AGE AND ORIGIN OP THE NIMROD GROUP AND OF THE GRANITE HARBOUR INTRUSIVES, BEARDMORE GLACIER REGION, 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 John Duncan Gunner, 3.A., M.A ****** The Ohio State University 1971 Approved by Adviser Department of Geology PLEASE NOTE: Some Pages have indistinct p rin t. Filmed as received. UNIVERSITY MICROFILMS igure 1: View across the Beardmore Glacier from the Summit of Mount Kyffin. The Rocks in the Foreground are Argillites and Arenites of the 'Goldie Formation, and the Sharp Peak is formed of Hope Granite. The Rounded Mountain on the Left Horizon is The Cloudmaker. ACKNOWLEDGMENTS I am greatly indebted to Dr. Gunter Faure for his enthusiastic ad vice and encouragement throughout this study. I am grateful also to the members of the Institute of Polar Studies expeditions to the Beardmore Glacier region during the 1967-1968 and 1969-1970 field seasons, and especially to David Johnston and to Drs. I. C. Rust and D. H. Elliot for willing assistance and stimulating dis cussions in the field. Logistic field support was provided by Squadron VXE-6 of the U. S. Naval Support Force, Antarctica, without whose help this study would not have been possible. -
Tulaczyk (PDF)
Journal of Glaciology, Vol. 55, No. 192, 2009 573 An inventory of active subglacial lakes in Antarctica detected by ICESat (2003–2008) Benjamin E. SMITH,1 Helen A. FRICKER,2 Ian R. JOUGHIN,1 Slawek TULACZYK3 1Applied Physics Laboratory, University of Washington, 1013 NE 40th Street, Box 355640, Seattle, Washington 98105-6698, USA E-mail: [email protected] 2Institute of Geophysics and Planetary Physics, Scripps Institution of Oceanography, University of California–San Diego, La Jolla, California 92093-0225, USA 3Department of Earth and Planetary Sciences, University of California Santa Cruz, Santa Cruz, California 95064, USA ABSTRACT. Through the detection of surface deformation in response to water movement, recent satellite studies have demonstrated the existence of subglacial lakes in Antarctica that fill and drain on timescales of months to years. These studies, however, were confined to specific regions of the ice sheet. Here we present the first comprehensive study of these ‘active’ lakes for the Antarctic ice sheet north of 868 S, based on 4.5 years (2003–08) of NASA’s Ice, Cloud and land Elevation Satellite (ICESat) laser altimeter data. Our analysis has detected 124 lakes that were active during this period, and we estimate volume changes for each lake. The ICESat-detected lakes are prevalent in coastal Antarctica, and are present under most of the largest ice-stream catchments. Lakes sometimes appear to transfer water from one to another, but also often exchange water with distributed sources undetectable by ICESat, suggesting that the lakes may provide water to or withdraw water from the hydrologic systems that lubricate glacier flow. -
U.S. Navy Antarctic Development Squadron Six Activities, 1984-1985
U.S. Navy Antarctic Development squadron had opened New Zealand's Vanda Station, Byrd sur- face camp, and South Pole Station. Squadron Six activities, 1984-1985 For the LC-130's, the season was characterized by a large increase in open-field work, the bulk of which was conducted for the combined glaciological programs at the Siple Coast. CDR. D.D. FISHER Other open-field projects included: (1) geological studies at the Jones Mountains, Ellsworth Mountains, and Mount Smart; (2) U.S. Navy Antarctic Development Squadron Six search for meteorites at Allan Hills; (3) volcanic research at Point Mugu, California 93042 Mount Takahe; (4) geologic/geochemical, stratigraphic, and sedimentological study of the English Coast on the Bell- ingshausen Sea; (5) ice-core retrieval and climatic research at the During the 1984-1985 austral summer, Antarctic Develop- Dominion Range, Transantarctic Mountains; (6) Federal Re- ment Six (VXE-6) marked its 30th year of providing air support public of Germany/United States/New Zealand North Victoria for the U.S. Antarctic Research Program. VXE-6 flight opera- Land Cooperative Program; (7) Antarctic Treaty Symposium at tions in Antarctica during the 1985 season were an unqualified the Lennox-King Glacier; (8) stratigraphic evolution and tec- success, with all logistics tasking completed on or ahead of tonic setting research, Ross Sequence, Transantarctic Moun- schedule. tains and Nimrod and Starshot Glaciers. During an attempt to The season began on 15 August 1984 when three ski- relocate the field camp at the Starshot Glacier, one LC-130, XD- equipped Hercules (Lc-130's) departed their home station in 02, was trapped in a crevasse and was severely damaged. -
1 Compiled by Mike Wing New Zealand Antarctic Society (Inc) Volume 1-36: Feb 2019 Vessel Names Are Shown Viz: “Aconcagua”. S
ANTARCTIC1 Compiled by Mike Wing 12: 190, 19: 144, 22: 5, New Zealand Antarctic Society (Inc) Injury, 1: 340, 2: 118, 492, 3: 480, 509, 523, 4: 15, 8: 130, 282, 315, 317, 331, 409, Volume 1-36: Feb 2019 9: 12, 18, 19, 23, 125, 313, 394, 6: 17, 7: 6, 22, 11: 395, 12: 348, 18: 56, 19: 95, Vessel names are shown viz: “Aconcagua”. See also 22: 16, 32: 29, list of ship names under ‘Ships’. Ships All book reviews are shown under ‘Book Reviews’ ANARE, 8: 13, All Universities are shown under ‘Universities’ Argentine Navy, 1: 336, Aircraft types appear under ‘Aircraft’. “Bahia Paraiso” Obituaries & Tributes are shown under 'Obituaries', see Sinking 11: 384, 391, 441, 476, 12: 22, 200, also individual names. 353, 13: 28, Fishing, 30: 1, Vol 20 page numbers 27-36 are shared by both double Japanese, 24: 67, issues 1&2 and 3&4. Those in double issue 3&4 are NGO, 29, 62(issue 4), marked accordingly viz: 20: 4 (issue 3&4) Polar, 34, Soviet, 8: 426, Vol 27 page numbers 1-20 are shared by both issues Tourist ships, 20: 58, 62, 24: 67, 1&2. Those in issue 2 are marked accordingly viz. 27: Vehicles, (issue 2) NZ Snow-cat, 2: 118, US bulldozer, 1: 202, 340, 12: 54, Vol 29 pages 62-68 are shared by both issues 3&4. ACECRC, see Antarctic Climate & Ecosystems Duplicated pages in 4 are marked accordingly viz. 63: Cooperation Research Centre (issue 4). Acevedo, Capitan. A.O. 4: 36, Ackerman, Piers, 21: 16, Ackroyd, Lieut. -
Structural Provinces of the Ross Ice Shelf, Antarctica
Annals of Glaciology 58(75pt1) 2017 doi: 10.1017/aog.2017.24 88 © The Author(s) 2017. This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons. org/licenses/by/4.0/), which permits unrestricted re-use, distribution, and reproduction in any medium, provided the original work is properly cited. Structural provinces of the Ross Ice Shelf, Antarctica Christine M. LEDOUX,1 Christina L. HULBE,2 Martin P. FORBES,2 Ted A. SCAMBOS,3 Karen ALLEY3 1Department of Geology, Portland State University, Portland, OR 97215, USA 2School of Surveying, University of Otago, Dunedin, New Zealand. E-mail: [email protected] 3National Snow and Ice Data Center, University of Colorado Boulder, Boulder, CO, USA ABSTRACT. The surface of the Ross Ice Shelf (RIS) is textured by flow stripes, crevasses and other fea- tures related to ice flow and deformation. Here, moderate resolution optical satellite images are used to map and classify regions of the RIS characterized by different surface textures. Because the textures arise from ice deformation, the map is used to identify structural provinces with common deformation history. We classify four province types: regions associated with large outlet glaciers, shear zones, exten- sion downstream of obstacles and suture zones between provinces with different upstream sources. Adjacent provinces with contrasting histories are in some locations deforming at different rates, suggest- ing that our province map is also an ice fabric map. Structural provinces have more complicated shapes in the part of the ice shelf fed by West Antarctic ice streams than in the part fed by outlet glaciers from the Transantarctic Mountains. -
Accepted Manuscript1.0
Quaternary Science Reviews 159 (2017) 88e102 Contents lists available at ScienceDirect Quaternary Science Reviews journal homepage: www.elsevier.com/locate/quascirev East Antarctic ice sheet stability recorded in a high-elevation ice-cored moraine * Nicole A. Bader a, Kathy J. Licht a, , Michael R. Kaplan b, Christine Kassab a, Gisela Winckler b a Department of Earth Sciences, Indiana University-Purdue University Indianapolis, Indianapolis, IN, USA b Lamont-Doherty Earth Observatory, Palisades, NY, USA article info abstract Article history: Till in an extensive blue ice moraine in the central Transantarctic Mountains at Mt. Achernar shows Received 12 August 2016 relatively continuous deposition by East Antarctic derived ice throughout the last glacial cycle. The most Received in revised form recently exposed material along the active margin of the Law Glacier (Zone 1) has hummocky topog- 2 December 2016 raphy that transitions into to a relatively flat region (Zone 2), followed by a series of ~2 m high Accepted 7 December 2016 continuous, parallel/sub-parallel ridges and troughs (Zones 3e5). The entire moraine is ice-cored. Past surface changes of <40 m are indicated by a lateral moraine at the base of Mt. Achernar and substantial topographic relief across Zone 3. Keywords: Provenance Pebble lithology and detrital zircon geochronology were analyzed on samples along a 6.5 km transect Outlet glacier across the moraine which formed from sub- and englacial debris. Beacon and Ferrar Supergroup rocks Detrital zircon comprise most rock types on the moraine surface. Overall, pebbles in Zones 1, 4 and 5 are dominated by Till igneous rocks of the Ferrar dolerite, whereas Zones 2 and 3 have ~40% more Beacon Supergroup sedi- Lithology mentary rocks. -
Gazetteer of the Antarctic
NOIJ.VQNn OJ3ON3133^1 VNOI±VN r o CO ] ] Q) 1 £Q> : 0) >J N , CO O The National Science Foundation has TDD (Telephonic Device for the Deaf) capability, which enables individuals with hearing impairment to communicate with the Division of Personnel and Management about NSF programs, employment, or general information. This number is (202) 357-7492. GAZETTEER OF THE ANTARCTIC Fourth Edition names approved by the UNITED STATES BOARD ON GEOGRAPHIC NAMES a cooperative project of the DEFENSE MAPPING AGENCY Hydrographic/Topographic Center Washington, D. C. 20315 UNITED STATES GEOLOGICAL SURVEY National Mapping Division Reston, Virginia 22092 NATIONAL SCIENCE FOUNDATION Division of Polar Programs Washington, D. C. 20550 1989 STOCK NO. GAZGNANTARCS UNITED STATES BOARD ON GEOGRAPHIC NAMES Rupert B. Southard, Chairman Ralph E. Ehrenberg, Vice Chairman Richard R. Randall, Executive Secretary Department of Agriculture .................................................... Sterling J. Wilcox, member Donald D. Loff, deputy Anne Griesemer, deputy Department of Commerce .................................................... Charles E. Harrington, member Richard L. Forstall, deputy Henry Tom, deputy Edward L. Gates, Jr., deputy Department of Defense ....................................................... Thomas K. Coghlan, member Carl Nelius, deputy Lois Winneberger, deputy Department of the Interior .................................................... Rupert B. Southard, member Tracy A. Fortmann, deputy David E. Meier, deputy Joel L. Morrison, deputy Department -
Geochemical Zones and Environmental Gradients for Soils from the 2 Central Transantarctic Mountains, Antarctica
1 Geochemical zones and environmental gradients for soils from the 2 Central Transantarctic Mountains, Antarctica 3 Melisa A. Diaz1,2†*, Christopher B. Gardner1,2, Susan A. Welch1,2, W. Andrew Jackson3, Byron J. 4 Adams4, Diana H. Wall5, Ian D. Hogg6,7, Noah Fierer8, W. Berry Lyons1,2 5 1School of Earth Sciences, The Ohio State University, Columbus, OH, USA 6 2Byrd Polar and Climate Research Center, The Ohio State University, Columbus, OH, USA 7 3Department of Civil, Environmental, & Construction Engineering, Texas Tech University, Lubbock, TX, USA 8 4Department of Biology, Evolutionary Ecology Laboratories, and Monte L. Bean Museum, Brigham Young University, 9 Provo, UT, USA 10 5Department of Biology and School of Global Environmental Sustainability, Colorado State University, Fort Collins, CO, 11 USA 12 6Canadian High Arctic Research Station, Polar Knowledge Canada, Cambridge Bay, Nunavut, Canada 13 7School of Science, University of Waikato, Hamilton, New Zealand 14 8Department of Ecology and Evolutionary Biology and Cooperative Institute for Research in Environmental Science, 15 University of Colorado Boulder, Boulder, CO, USA 16 17 †Now at Departments of Geology and Geophysics and Applied Ocean Physics and Engineering, Woods Hole Oceanographic 18 Institution, Woods Hole, MA, USA 19 20 Correspondence to: Melisa A. Diaz ([email protected]) 21 22 Abstract. Previous studies have established links between biodiversity and soil geochemistry in the McMurdo Dry Valleys, 23 Antarctica, where environmental gradients are important determinants of soil biodiversity. However, these gradients are not 24 well established in the Central Transantarctic Mountains, which are thought to represent some of the least hospitable 25 Antarctic soils. We analyzed 220 samples from 11 ice-free areas along the Shackleton Glacier (~85 °S), a major outlet 26 glacier of the East Antarctic Ice Sheet. -
Workshop on Antarctic Glaciology and Meteorites
WORKSHOP ON ANTARCTIC GLACIOLOGY AND METEORITES ....fa o LPI Technical Report Number 82-03 FS LUNAR AND PLANETARY INSTITUTE 3303 NASA ROAD 1 HOUSTON, TEXAS 77058 WORKSHOP ON ANTARCTIC GLACIOLOGY AND METEORITES by: Colin Bull and Michael E. Lipschutz Sponsored by The Lunar and Planetary Institute April 19-21, 1982 Lunar and Planetary Institute 3303 NASA Road 1 Houston, Texas 77058 LPI Technical Report 82-03 Compiled in 1982 by the LUNAR AND PLANETARY INSTITUTE The Institute is operated by Universities Space Research Association under Contract NASW-3389 with the National Aeronautics and Space Administration. Material in this document may be copied without restraint for library, abstract service, educational or personal research purposes; however, republication of any portion requires the written permission of the authors as well as appropriate acknowledgment of this publication. This report may be cited as: Bull, C. and Lipschutz, M. (1982) Workshop on Antarctic Glaciology and Meteorites. LPI Tech. Rpt. 82-03. Lunar and Planetary Institute, Houston. 57 pp. Papers in this report may be cited as: Author A. (1982) Title of part. In Workshop on Antarctic Glaciology and Meteorites (Bull, C. and Lipschutz, M.), p. xx-yy. LPI Tech. Rpt. 82-03. Lunar and Planetary Institute, Houston. This report is distributed by: L1BRARY/INFORMATION CENTER Lunar and Planetary Institute 3303 NASA Road I Houston, TX 77058 Mail order requestors will be invoiced for the cost of postage and handling. Contents I. Introduction 1 II. Program 4 III. Discussion 6 IV. Recommendations 24 Appendix I: Abstracts 27 Characterization of antarctic meteorites 29 Brian Mason Antarctic meteorites: Some new problems and opportunities 31 W. -
Erifinal2018.Pdf
The Wyckoff Educational Commission would like to thank the following committee members, organizations and individuals for their vital assistance in preparing our latest Environmental Resource Inventory of Wyckoff. 2018 Environmental Resources Inventory Sub-Committee Julia Alfano, Green Team Student Volunteer Denise Capparelli, Environmental Commissioner Robert Fortunato, Planning Board Liaison/Environmental Commissioner JR. Frank, Green Team Volunteer Christine Key, Environmental Commissioner Thomas J. Madigan, Township Committeeman and Environmental Commission Liaison John McCauley, Environmental Commission Chairman Contributing Organizations Partners in Pride Climate Mama Wyckoff Area Garden Club Wyckoff Historical Society Wyckoff Shade Tree Commission Wyckoff Building Department Individuals Robert Shannon, Wyckoff Township Administrator Harriet Shugarman, Founder and Executive Director, Climate Mama Susan Litt, President, Partners in Pride Janet Schuls, Master Gardener, Class of 1988 Michael Mitchell, NJ Rosarian Peter Weiderhold, Past Chair, Wyckoff Environmental Commission and Green Team Volunteer Cindy Risseeuw, Technical Assistant, Wyckoff Building Department Ira Lakritz, Wyckoff Bird Photographer Special thanks and appreciation to Denise Capparelli, Environmental Commissioner, for administering and preparation of the new Environmental Resources Inventory. Special thanks to the Wyckoff Library for providing meeting accommodations The Wyckoff Environmental Commission would like to acknowledge the previous committee, Partners in