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• W2100043447 abstract "Research Article| January 01, 2014 The Ellsworth Subglacial Highlands: Inception and retreat of the West Antarctic Ice Sheet Neil Ross; Neil Ross † 1School of Geography, Politics and Sociology, Newcastle University, Newcastle upon Tyne, NE1 7RU, UK †E-mail: neil.ross@ncl.ac.uk Search for other works by this author on: GSW Google Scholar Tom A. Jordan; Tom A. Jordan 2British Antarctic Survey, Cambridge CB3 0ET, UK Search for other works by this author on: GSW Google Scholar Robert G. Bingham; Robert G. Bingham 3School of Geosciences, University of Edinburgh, Edinburgh EH8 9XP, UK Search for other works by this author on: GSW Google Scholar Hugh F.J. Corr; Hugh F.J. Corr 2British Antarctic Survey, Cambridge CB3 0ET, UK Search for other works by this author on: GSW Google Scholar Fausto Ferraccioli; Fausto Ferraccioli 2British Antarctic Survey, Cambridge CB3 0ET, UK Search for other works by this author on: GSW Google Scholar Anne Le Brocq; Anne Le Brocq 4School of Geography, University of Exeter, Exeter EX4 4RJ, UK Search for other works by this author on: GSW Google Scholar David M. Rippin; David M. Rippin 5Environment Department, University of York, York YO10 5DD, UK Search for other works by this author on: GSW Google Scholar Andrew P. Wright; Andrew P. Wright 4School of Geography, University of Exeter, Exeter EX4 4RJ, UK Search for other works by this author on: GSW Google Scholar Martin J. Siegert Martin J. Siegert 6Bristol Glaciology Centre, School of Geographical Sciences, University of Bristol, Bristol BS8 1SS, UK Search for other works by this author on: GSW Google Scholar GSA Bulletin (2014) 126 (1-2): 3–15. https://doi.org/10.1130/B30794.1 Article history received: 20 Sep 2012 rev-recd: 27 Feb 2013 accepted: 01 Mar 2013 first online: 08 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Neil Ross, Tom A. Jordan, Robert G. Bingham, Hugh F.J. Corr, Fausto Ferraccioli, Anne Le Brocq, David M. Rippin, Andrew P. Wright, Martin J. Siegert; The Ellsworth Subglacial Highlands: Inception and retreat of the West Antarctic Ice Sheet. GSA Bulletin 2014;; 126 (1-2): 3–15. doi: https://doi.org/10.1130/B30794.1 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGSA Bulletin Search Advanced Search Abstract Antarctic subglacial highlands are where the Antarctic ice sheets first developed and the “pinning points” where retreat phases of the marine-based sectors of the ice sheet are impeded. Due to low ice velocities and limited present-day change in the ice-sheet interior, West Antarctic subglacial highlands have been overlooked for detailed study. These regions have considerable potential, however, for establishing the locations from which the West Antarctic Ice Sheet originated and grew, and its likely response to warming climates. Here, we characterize the subglacial morphology of the Ellsworth Subglacial Highlands, West Antarctica, from ground-based and aerogeophysical radio-echo sounding (RES) surveys and the Moderate-Resolution Imaging Spectroradiometer (MODIS) Mosaic of Antarctica. We document well-preserved classic landforms associated with restricted, dynamic, marine-proximal alpine glaciation, with hanging tributary valleys feeding a significant overdeepened trough (the Ellsworth Trough) cut by valley (tidewater) glaciers. Fjord-mouth threshold bars down-ice of two overdeepenings define both the northwest and southeast termini of paleo-outlet glaciers, which cut and occupied the Ellsworth Trough. Satellite imagery reveals numerous other glaciated valleys, terminating at the edge of deep former marine basins (e.g., Bentley Subglacial Trench), throughout the Ellsworth Subglacial Highlands. These geomorphic data can be used to reconstruct the glaciology of the ice masses that formed the proto–West Antarctic Ice Sheet. The landscape predates the present ice sheet and was formed by a small dynamic ice field(s), similar to those of the present-day Antarctic Peninsula, at times when the marine sections of the West Antarctic Ice Sheet were absent. The Ellsworth Subglacial Highlands represent a major seeding center of the paleo–West Antarctic Ice Sheet, and its margins represent the pinning point at which future retreat of the marine-based West Antarctic Ice Sheet would be arrested. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
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• W2100043447 date "2013-09-19" @default.
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• W2100043447 title "The Ellsworth Subglacial Highlands: Inception and retreat of the West Antarctic Ice Sheet" @default.
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