Grounding-zone wedges and mega-scale glacial lineations in Kveithola Trough, Barents Sea
Atlas of Submarine Glacial Landforms: Modern, Quaternary and Ancient.-- 2 pages, 1 figures Multibeam-bathymetric data from Kveithola Trough show a seafloor characterized by east–west-trending mega-scale glacial lineations (MSGLs) overprinted by transverse grounding-zone wedges (GZWs). GZWs are thoug...
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Online Access: | http://hdl.handle.net/10261/143604 https://doi.org/10.1144/M46.32 |
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ftcsic:oai:digital.csic.es:10261/143604 2024-02-11T10:02:27+01:00 Grounding-zone wedges and mega-scale glacial lineations in Kveithola Trough, Barents Sea Rebesco, Michele Urgeles, Roger Özmaral, A. Llopart, Jaume CORIBAR Scientific Party 2016 http://hdl.handle.net/10261/143604 https://doi.org/10.1144/M46.32 unknown Geological Society of London https://dx.doi.org/10.1144/M46.32 Sí doi:10.1144/M46.32 issn: 0435-4052 e-issn: 2041-4722 Memoirs 46: 231-232 (2016) http://hdl.handle.net/10261/143604 none artículo http://purl.org/coar/resource_type/c_6501 2016 ftcsic https://doi.org/10.1144/M46.32 2024-01-16T10:20:18Z Atlas of Submarine Glacial Landforms: Modern, Quaternary and Ancient.-- 2 pages, 1 figures Multibeam-bathymetric data from Kveithola Trough show a seafloor characterized by east–west-trending mega-scale glacial lineations (MSGLs) overprinted by transverse grounding-zone wedges (GZWs). GZWs are thought to form by deposition of subglacial till at temporarily stable ice-sheet marine termini between successive episodic retreats (Batchelor & Dowdeswell 2015). Sub-bottom profiles show that the present-day morphology of Kveithola Trough is largely inherited from the palaeo-seafloor topography of the GZWs, which is now draped by deglacial to early Holocene glacimarine sediment about 15 m thick. The ice stream that produced such subglacial morphology was flowing from east to west towards the shelf edge in Kveithola Trough during the Last Glacial Maximum (LGM). Its rapid retreat was probably associated with progressive lift-off and successive rapid melting of grounded ice induced by eustatic sea-level rise Peer Reviewed Article in Journal/Newspaper Barents Sea Ice Sheet Digital.CSIC (Spanish National Research Council) Barents Sea Geological Society, London, Memoirs 46 1 231 232 |
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Digital.CSIC (Spanish National Research Council) |
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ftcsic |
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Atlas of Submarine Glacial Landforms: Modern, Quaternary and Ancient.-- 2 pages, 1 figures Multibeam-bathymetric data from Kveithola Trough show a seafloor characterized by east–west-trending mega-scale glacial lineations (MSGLs) overprinted by transverse grounding-zone wedges (GZWs). GZWs are thought to form by deposition of subglacial till at temporarily stable ice-sheet marine termini between successive episodic retreats (Batchelor & Dowdeswell 2015). Sub-bottom profiles show that the present-day morphology of Kveithola Trough is largely inherited from the palaeo-seafloor topography of the GZWs, which is now draped by deglacial to early Holocene glacimarine sediment about 15 m thick. The ice stream that produced such subglacial morphology was flowing from east to west towards the shelf edge in Kveithola Trough during the Last Glacial Maximum (LGM). Its rapid retreat was probably associated with progressive lift-off and successive rapid melting of grounded ice induced by eustatic sea-level rise Peer Reviewed |
format |
Article in Journal/Newspaper |
author |
Rebesco, Michele Urgeles, Roger Özmaral, A. Llopart, Jaume CORIBAR Scientific Party |
spellingShingle |
Rebesco, Michele Urgeles, Roger Özmaral, A. Llopart, Jaume CORIBAR Scientific Party Grounding-zone wedges and mega-scale glacial lineations in Kveithola Trough, Barents Sea |
author_facet |
Rebesco, Michele Urgeles, Roger Özmaral, A. Llopart, Jaume CORIBAR Scientific Party |
author_sort |
Rebesco, Michele |
title |
Grounding-zone wedges and mega-scale glacial lineations in Kveithola Trough, Barents Sea |
title_short |
Grounding-zone wedges and mega-scale glacial lineations in Kveithola Trough, Barents Sea |
title_full |
Grounding-zone wedges and mega-scale glacial lineations in Kveithola Trough, Barents Sea |
title_fullStr |
Grounding-zone wedges and mega-scale glacial lineations in Kveithola Trough, Barents Sea |
title_full_unstemmed |
Grounding-zone wedges and mega-scale glacial lineations in Kveithola Trough, Barents Sea |
title_sort |
grounding-zone wedges and mega-scale glacial lineations in kveithola trough, barents sea |
publisher |
Geological Society of London |
publishDate |
2016 |
url |
http://hdl.handle.net/10261/143604 https://doi.org/10.1144/M46.32 |
geographic |
Barents Sea |
geographic_facet |
Barents Sea |
genre |
Barents Sea Ice Sheet |
genre_facet |
Barents Sea Ice Sheet |
op_relation |
https://dx.doi.org/10.1144/M46.32 Sí doi:10.1144/M46.32 issn: 0435-4052 e-issn: 2041-4722 Memoirs 46: 231-232 (2016) http://hdl.handle.net/10261/143604 |
op_rights |
none |
op_doi |
https://doi.org/10.1144/M46.32 |
container_title |
Geological Society, London, Memoirs |
container_volume |
46 |
container_issue |
1 |
container_start_page |
231 |
op_container_end_page |
232 |
_version_ |
1790598396850995200 |