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• W1972738781 abstract "Research Article| January 01, 2004 Thickness and extent of the subglacial till layer beneath an Antarctic paleo–ice stream Julian A. Dowdeswell; Julian A. Dowdeswell 1Scott Polar Research Institute, University of Cambridge, Cambridge CB2 1ER, UK Search for other works by this author on: GSW Google Scholar Colm Ó Cofaigh; Colm Ó Cofaigh 1Scott Polar Research Institute, University of Cambridge, Cambridge CB2 1ER, UK Search for other works by this author on: GSW Google Scholar Carol J. Pudsey Carol J. Pudsey 2British Antarctic Survey, High Cross, Madingley Road, Cambridge CB3 0ET, UK Search for other works by this author on: GSW Google Scholar Author and Article Information Julian A. Dowdeswell 1Scott Polar Research Institute, University of Cambridge, Cambridge CB2 1ER, UK Colm Ó Cofaigh 1Scott Polar Research Institute, University of Cambridge, Cambridge CB2 1ER, UK Carol J. Pudsey 2British Antarctic Survey, High Cross, Madingley Road, Cambridge CB3 0ET, UK Publisher: Geological Society of America Received: 23 May 2003 Revision Received: 05 Sep 2003 Accepted: 08 Sep 2003 First Online: 09 Mar 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 Geological Society of America Geology (2004) 32 (1): 13–16. https://doi.org/10.1130/G19864.1 Article history Received: 23 May 2003 Revision Received: 05 Sep 2003 Accepted: 08 Sep 2003 First Online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Tools Icon Tools Get Permissions Search Site Citation Julian A. Dowdeswell, Colm Ó Cofaigh, Carol J. Pudsey; Thickness and extent of the subglacial till layer beneath an Antarctic paleo–ice stream. Geology 2004;; 32 (1): 13–16. doi: https://doi.org/10.1130/G19864.1 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 SocietyGeology Search Advanced Search Abstract Fast-flowing ice streams and outlet glaciers currently account for as much as 90% of the discharge from the Antarctic and Greenland Ice Sheets. Although the deformation of subglacial material has been proposed as the mechanism for this rapid motion, such sediment is usually hidden under several kilometers of ice. Marine-geophysical records have allowed reconstruction of the three-dimensional thickness of the sedimentary bed beneath a large Antarctic paleo–ice stream for the first time. Fast flow is indicated by streamlined seafloor lineations that form the surface of a layer of low shear strength, unsorted sediment, averaging 4.6 m thick. Rapid motion of the paleo–ice stream was a result of subglacial deformation within this layer. 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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• W1972738781 title "Thickness and extent of the subglacial till layer beneath an Antarctic paleo–ice stream" @default.
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