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Late Quaternary Surface Fluctuations of Beardmore Glacier, Antarctica
Late Quaternary surface fluctuations Journal, this issue). These four drifts are from 10 centimeters to several meters thick. They are composed largely of unconsoli- of Beardmore Glacier, Antarctica dated gravel. Numerous included striated clasts were probably reworked from Sirius drift. Thin boulder-belt moraines com- monly mark drift surfaces and define outer edges of drift sheets. The thin drift sheets overlie well-preserved morphological fea- tures, particularly in Sirius deposits. Figure 3 shows former surfaces of Beardmore Glacier repre- G. H. DENTON sented by the four drift sheets. The upper limit of Plunket drift parallels the present surface of Beardmore Glacier along its Institute for Quaternary Studies entire length. It also fringes the snout of Rutkowski Glacier, and which drains the local ice cap on the Dominion Range. This drift Department of Geological Sciences configuration shows similar behavior of these two glaciers dur- University of Maine Orono, Maine 04469 ing deposition of Plunket drift. The upper limit of Beardmore and Meyer drifts are close to the present surface of Beardmore Glacier near the polar plateau but systematically rise above the B.C. ANDERSEN present surface in the downglacier direction. Further, the areal patterns of Beardmore and Meyer drifts show recession of Department of Geology Rutkowski Glacier concurrent with expansion of Beardmore University of Oslo Glacier. Dominion drift occurs on the northern flank of the Oslo, Noruay Dominion Range, where it reaches high above Beardmore Glacier (Prentice et al., Antarctic Journal, this issue). We draw several inferences from the configuration, physical H.W. CONWAY characteristics, and weathering of these four drift sheets. -
The Dominion Range Ice Core, Queen Maud Mountains, Antarctica - General Site and Core Characteristics with Implications
Journal of Glaciology, Vo!. 36, No. 122, 1990 THE DOMINION RANGE ICE CORE, QUEEN MAUD MOUNTAINS, ANTARCTICA - GENERAL SITE AND CORE CHARACTERISTICS WITH IMPLICATIONS By PAUL A. MAYEWSKI, MARK S. TWICKLER, WM BERRY LYONS, MARY 10 SPENCER, (Glacier Research Group, Institute for the Study of Earth, Oceans and Space (EOS), University of New Hampshire, Durham, New Hampshire 03824, U.S.A.) DEBRA A. MEESE, (Glacier Research Group, Institute for the Study of Earth, Oceans and Space (EOS), University of New Hampshire, Durham, New Hampshire 03824, U.S.A., and U.S. Army Cold Regions Research and Engineering Laboratory, Hanover, New Hampshire 03755, U.S.A.) ANTHONY 1. Gow, (U.S. Army Cold Regions Research and Engineering Laboratory, Hanover, New Hampshire 03755, U.S.A.) PIETER GROOTES, (Quaternary Isotope Laboratory, University of Washington, Seattle, Washington 98195, U.S.A.) TODD SO W ERS, (Graduate School of Oceanography, University of Rhode Island, Narragansett, Rhode Island 02882, U.S.A.) M. SCOTT WATSON, (Polar Ice Coring Office, University of Nebraska, Lincoln, Nebraska 68558, U.S.A.) and ERIC SALTZMAN (Rosenstiel School of Marine and Atmospheric Sciences, University of Miami, Miami, Florida 33149, U.S.A.) ABSTRACT. The Transantarctic Mountains of East they could provide some of the most climatically sensitive Antarctica provide a new milieu for retrieval of ice-core records available from Antarctica. Furthermore, unlike records. We report here on the initial findings from the those ice cores retrieved from the interior of Antarctica, first of these records, the Dominion Range ice-core record. there are terrestrial records from nearby sites that can be Sites such as the Dominion Range are valuable for the used for comparison (e.g. -
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. -
Late Quaternary Terrestrial Processes, Sediments and History: from Glacial to Postglacial Environments
INQUA TERPRO COMMISSION PERIBALTIC WORKING GROUP UNIVERSITY OF LATVIA UNIVERSITY OF DAUGAVPILS LATVIAN ASSOCIATION FOR QUATERNARY RESEARCH LATE QUATERNARY TERRESTRIAL PROCESSES, SEDIMENTS AND HISTORY: FROM GLACIAL TO POSTGLACIAL ENVIRONMENTS EASTERN AND CENTRAL LATVIA AUGUST 17-22, 2014 EXCURSION GUIDE AND ABSTRACTS INQUA TEPRO COMMISSION PERIBALTIC WORKING GROUP UNIVERSITY OF LATVIA UNIVERSITY OF DAUGAVPILS LATVIAN ASSOCIATION FOR QUATERNARY RESEARCH LATE QUATERNARY TERRESTRIAL PROCESSES, SEDIMENTS AND HISTORY: FROM GLACIAL TO POSTGLACIAL ENVIRONMENTS EASTERN AND CENTRAL LATVIA AUGUST 16-22, 2014 EXCURSION GUIDE AND ABSTRACTS UNIVERSITY OF LATVIA RĪGA 2014 Organized by: University of Latvia Daugavpils University Latvian Association for Quaternary Research INQUA Peribaltic Working Group (INQUA TERPRO Commission) Organizing committee: Māris Nartišs (Chair, University of Latvia) Māris Krievāns (Secretary, University of Latvia) Aivars Markots (University of Latvia) Juris Soms (Daugavpils University) Evija Tērauda (University of Latvia) Vitālijs Zelčs (University of Latvia) Contributors: Ivars Celiņš, Edgars Greiškalns, Ieva Grudzinska, Edyta Kalińska-Nartiša, Laimdota Kalniņa, Jānis Karušs, Māris Krievāns, Kristaps Lamsters, Aivars Markots, Māris Nartišs, Agnis Rečs, Normunds Stivriņš, Juris Soms, Ivars Strautnieks, Santa Strode, Sandra Zeimule, Vitālijs Zelčs Editors: Vitālijs Zelčs and Māris Nartišs The English texts of the field guide were revised by Valdis Bērziņš Recommended reference for this publication: Zelčs, V. and Nartišs, M. -
Cloud Download
NASA Conference Publication 3115, Vol. 2 West Antarctic Ice Sheet Initiative Volume 2: Discipline Reviews Edited by Robert A. Bindschadler NASA Goddard Space Flight Center Greenbelt, Maryland Proceedings of a workshop cosponsored by the National Aeronautics and Space Administration, Washington, D.C., and the National Science Foundation, Washington, D.C., and held at Goddard Space Flight Center Greenbelt, Maryland October 16-18, 1990 National Aeronautics and Space Administration Qffice of Management Scientific and Technical Information Program 1991 PREFACE This report contains seven discipline review papers on the state of our knowledge of West Antarctica and opinions on how that knowledge must be increased to predict the future behavior of this ice sheet. The papers were prepared to accompany lectures given at the second SeaRISE workshop held October 16-18, 1990 at NASA/Goddard Space Flight Center in Greenbelt, Maryland. The purpose of the workshop was to draft a Science and Implementation Plan of what was once called SeaRISE but is now called the West Antarctic Ice Sheet Initiative (WAIS). This plan appears as Volume I of this proceedings series. iii PRECEDING PAGE BLANK NOT FILMED CONTENTS A Review of Precipitation-Related Aspects of West Antarctic Meteorology D.H. Bromwich, A.M. Carleton, and T.R. Parish ......................................... 1 Sea-Level Response to Ice Sheet Evolution: An Ocean Perspective S.S. Jacobs .............................................................................................. 23 Terrestrial Geophysics in the SeaRISE Project C.R. Bentley ............................................................................................. 49 Late Wisconsin and Early Holocene Glacial History, Inner Ross Embayment, Antarctica G.H. Denton, J.G. Bockheim, S.C. Wilson, and M. Stuiver ...................... 55 Marine Record of Late Quaternary Glacial-Interglacial Fluctuations in the Ross Sea and Evidence for Rapid, Episodic Sea Level Change Due to Marine Ice Sheet Collapse J.B. -
The Dominion Range Ice Core Ter Understanding of Glacial Geologic Records
The University of Maine DigitalCommons@UMaine Earth Science Faculty Scholarship Earth Sciences 1986 The ominionD Range Ice Core Paul Andrew Mayewski University of Maine, [email protected] Follow this and additional works at: https://digitalcommons.library.umaine.edu/ers_facpub Part of the Geochemistry Commons, Geomorphology Commons, Glaciology Commons, and the Hydrology Commons Repository Citation Mayewski, Paul Andrew, "The ominionD Range Ice Core" (1986). Earth Science Faculty Scholarship. 223. https://digitalcommons.library.umaine.edu/ers_facpub/223 This Article is brought to you for free and open access by DigitalCommons@UMaine. It has been accepted for inclusion in Earth Science Faculty Scholarship by an authorized administrator of DigitalCommons@UMaine. For more information, please contact [email protected]. The Dominion Range ice core ter understanding of glacial geologic records. The most valuable ice-core records are those which are highly detailed and involve a number of different types of physical and chemical measure- ments because such records maximize the dating of the core while also providing the tightest resolution and interpretation. P.A. MAYEWSKI During the 1984-1985 austral summer, we undertook a field program on the plateau of the Dominion Range (figures 1 and Glacier Research Group 2), a localized accumulation basin at the head of the Beardmore and Glacier, Transantarctic Mountains. Studies conducted during Institute for the Study of Earth, Oceans and Space the field program included: (1) -
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12-12020-mg Doc 6436 Filed 02/05/14 Entered 02/05/14 19:53:19 Main Document Pg 1 of 169 UNITED STATES BANKRUPTCY COURT SOUTHERN DISTRICT OF NEW YORK ----------------------------------------------------x : In re : Chapter 11 : RESIDENTIAL CAPITAL, LLC, et al., 1 : Case No. 12-12020 (MG) : : : (Jointly Administered) Debtors. : ----------------------------------------------------x AFFIDAVIT OF SERVICE I, Clarissa D. Cu, depose and say that I am employed by Kurtzman Carson Consultants LLC (KCC), the claims and noticing agent for the Debtors. A. On January 29, 2014, at my direction and under my supervision, employees of KCC caused the following document to be served via Electronic Mail upon the Monthly Service List attached hereto Exhibit A, and via First Class Mail upon the service list attached hereto as Exhibit B and the Special Service List attached hereto as Exhibit C: Order Under 11 U.S.C. §§ 105(a) and 554(a) Approving Abandonment of Debtors' Interests in Certain Estate Assets [Docket No. 6380] B. Additionally, on January 29, 2014, at my direction and under my supervision, employees of KCC caused the following document to be served via Electronic Mail upon the Monthly Service List attached hereto Exhibit A and the service list attached hereto as Exhibit D, via Overnight Mail upon the service list attached hereto as Exhibit E, and via First Class Mail upon the Special Service List attached hereto as Exhibit C: 1 The Debtors in these chapter 11 cases, along with the last four digits of each Debtor’s federal tax identification number, are: Residential Capital, LLC (0738); ditech, LLC (7228); DOA Holding Properties, LLC (4257); DOA Properties IX (Lots-Other), LLC (3274), EPRE LLC (7974); Equity Investment I, LLC (2797); ETS of Virginia, Inc. -
Dane County Treasurer 2010 Parcels That MAY Be Eligible for Lottery Credits in Dane County CITY of EDGERTON ACKER, ALAN N
Dane County Treasurer 2010 Parcels that MAY Be Eligible for Lottery Credits in Dane County CITY OF EDGERTON ACKER, ALAN N Parcel Number: 0512-344-7056-2 Parcel Address: 1342 SAVANNAH WOODS DR DEGRAND, KEVIN C DEGRAND, RACHEL M Parcel Number: 0512-344-7221-2 Parcel Address: 1324 CUMBERLAND DR GARCZYNSKI, KEVIN M GARCZYNSKI, JULIA J Parcel Number: 0512-344-7045-2 Parcel Address: 1336 SAVANNAH WOODS DR KOLLMANSBERGER, ZACHARIAH P HAASE, MEGAN P Parcel Number: 0512-344-7232-2 Parcel Address: 1332 CUMBERLAND DR LARSEN, EVAN R DEBILZEN, MOLLY M Parcel Number: 0512-344-7067-2 Parcel Address: 1350 SAVANNAH WOODS DR MENTINK, TYLER S MENTINK, GESINA M Parcel Number: 0512-344-7265-2 Parcel Address: 1356 CUMBERLAND DR ROBBINS, BRYAN L WILLIAMS, MELISSA G Parcel Number: 0512-344-7166-2 Parcel Address: 1333 SAVANNAH WOODS DR RUCK, DAVID J RUCK, RACHEL Parcel Number: 0512-344-7012-2 Parcel Address: 1312 SAVANNAH WOODS DR SATTERLEE, VICTOR T SATTERLEE, JULIE L Parcel Number: 0512-344-9855-2 Parcel Address: 208 THRONSON DR SIEDSCHLAG, JEFFREY T ATKINSON, ERIN M Parcel Number: 0512-344-7133-2 Parcel Address: 1357 SAVANNAH WOODS DR CITY OF FITCHBURG ADAMS, JOHN W GARDEBRECHT, JILL L Parcel Number: 0609-113-6029-2 Parcel Address: 5204 SNAPDRAGON TRL ADIX, MICHAEL A Parcel Number: 0609-152-3129-2 Parcel Address: 24 HALITE WAY ADOLPHSON, EDWARD J ADOLPHSON, JUDITH M Parcel Number: 0609-162-6599-1 Parcel Address: 5711 MODERNAIRE ST AGARWAL, ROBERT R DUREJA, PARUL Parcel Number: 0609-113-4366-2 Parcel Address: 5216 SNAPDRAGON TRL AHMAD, NIHAL NIHAL, MINAKSHI -
By Gregory P. Streveler by David A. Brew
UNITED STATES DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY IN COOPERATION WITH THE NATIONAL PARK SERVICE BIBLIOGRAPHY OF RESEARCH AND EXPLORATION IN THE GLACIER BAY REGION, SOUTHEASTERN ALASKA, 1798-1992 By Doris L. Howe U.S. Geological Survey Volunteer-for-Science U.S. National Park Service Volunteer-in-Park 5119 E. Harbor Drive Friday Harbor, WA 98250 and Box 67 Gustavus, AK 99826-0067 INCLUDING AN ANNOTATED BIBLIOGRAPHY OF UNPUBLISHED REPORTS By Gregory P. Streveler Box 94 Gustavus, AK 99826-0094 AND AN INTRODUCTION AND ACKNOWLEDGEMENTS SECTION By David A. Brew U.S. Geological Survey, MS 904 345 Middlefield Road Menlo Park, CA 94025-3591 OPEN-FILE REPORT 92-596 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards or with the North American Stratigraphic Code. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government Bibliography of Research and Exploration In the Glacier Bay Region, southeastern Alaska, 1798-1992 Doris L. Howe (Compiler) INTRODUCTION AND ACKNOWLEDGEMENTS By David A. Brew The entries in this bibliography span almost two centuries of the human history, scientific research, and exploration activities in the Glacier Bay region of southeastern Alaska (Fig. 1). The reports, articles, and maps listed cover a wide variety of topics, but they are all unified by one common concern. That concern is the quest for knowledge about all aspects of the region. Almost without exception, the scientists and others who have produced this material consider themselves privileged to have been part of that quest; it is their hope that this bibliography will aid in continuing and expanding comprehensive scientific studies in the region.