Assemblages of submarine landforms in the glacial troughs of the northern Barents Sea, east of Svalbard
The Barents Sea is a wide, relatively deep epicontinental sea consisting of shallower banks (c. 50–100 m depth) separated by broad, flat-bottomed troughs (c. 200–400 m depth) that radiate out towards its western and northern margins (Fig. 1a). These troughs have been excavated by grounded ice during...
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Online Access: | http://nora.nerc.ac.uk/id/eprint/515711/ https://doi.org/10.1144/M46.170 |
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ftnerc:oai:nora.nerc.ac.uk:515711 2023-05-15T15:38:05+02:00 Assemblages of submarine landforms in the glacial troughs of the northern Barents Sea, east of Svalbard Hogan, Kelly A. Dowdeswell, J. A. Noormets, R. Dowdeswell, J.A. Canals, M. Jakobsson, M. Todd, B.J. Dowdeswell, E.K. Hogan, K.A. 2016 http://nora.nerc.ac.uk/id/eprint/515711/ https://doi.org/10.1144/M46.170 unknown Geological Society of London Hogan, Kelly A. orcid:0000-0002-1256-8010 Dowdeswell, J. A.; Noormets, R. 2016 Assemblages of submarine landforms in the glacial troughs of the northern Barents Sea, east of Svalbard. In: Dowdeswell, J.A.; Canals, M.; Jakobsson, M.; Todd, B.J.; Dowdeswell, E.K.; Hogan, K.A. orcid:0000-0002-1256-8010 , (eds.) Atlas of submarine glacial landforms: modern, Quaternary and ancient. London, Geological Society of London, 333-336. (Geological Society Memoir, 46, 46). Publication - Book Section PeerReviewed 2016 ftnerc https://doi.org/10.1144/M46.170 2023-02-04T19:44:13Z The Barents Sea is a wide, relatively deep epicontinental sea consisting of shallower banks (c. 50–100 m depth) separated by broad, flat-bottomed troughs (c. 200–400 m depth) that radiate out towards its western and northern margins (Fig. 1a). These troughs have been excavated by grounded ice during multiple glaciations through the Plio-Pleistocene (Jakobsson et al. 2014). During the Last Glacial Maximum (LGM) the Barents Sea Ice Sheet (BSIS) extended across the entire northern Barents Sea to the shelf break (Svendsen et al. 2004; Jakobsson et al. 2014). Fast-flowing ice drained the ice sheet through these troughs and produced a suite of seafloor landforms that preserves both a record of former ice-flow patterns and of how the ice sheet retreated during deglaciation (Dowdeswell et al. 2010; Hogan et al. 2010a). Book Part Barents Sea Ice Sheet Sea ice Svalbard Natural Environment Research Council: NERC Open Research Archive Svalbard Barents Sea Geological Society, London, Memoirs 46 1 333 336 |
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Open Polar |
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Natural Environment Research Council: NERC Open Research Archive |
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ftnerc |
language |
unknown |
description |
The Barents Sea is a wide, relatively deep epicontinental sea consisting of shallower banks (c. 50–100 m depth) separated by broad, flat-bottomed troughs (c. 200–400 m depth) that radiate out towards its western and northern margins (Fig. 1a). These troughs have been excavated by grounded ice during multiple glaciations through the Plio-Pleistocene (Jakobsson et al. 2014). During the Last Glacial Maximum (LGM) the Barents Sea Ice Sheet (BSIS) extended across the entire northern Barents Sea to the shelf break (Svendsen et al. 2004; Jakobsson et al. 2014). Fast-flowing ice drained the ice sheet through these troughs and produced a suite of seafloor landforms that preserves both a record of former ice-flow patterns and of how the ice sheet retreated during deglaciation (Dowdeswell et al. 2010; Hogan et al. 2010a). |
author2 |
Dowdeswell, J.A. Canals, M. Jakobsson, M. Todd, B.J. Dowdeswell, E.K. Hogan, K.A. |
format |
Book Part |
author |
Hogan, Kelly A. Dowdeswell, J. A. Noormets, R. |
spellingShingle |
Hogan, Kelly A. Dowdeswell, J. A. Noormets, R. Assemblages of submarine landforms in the glacial troughs of the northern Barents Sea, east of Svalbard |
author_facet |
Hogan, Kelly A. Dowdeswell, J. A. Noormets, R. |
author_sort |
Hogan, Kelly A. |
title |
Assemblages of submarine landforms in the glacial troughs of the northern Barents Sea, east of Svalbard |
title_short |
Assemblages of submarine landforms in the glacial troughs of the northern Barents Sea, east of Svalbard |
title_full |
Assemblages of submarine landforms in the glacial troughs of the northern Barents Sea, east of Svalbard |
title_fullStr |
Assemblages of submarine landforms in the glacial troughs of the northern Barents Sea, east of Svalbard |
title_full_unstemmed |
Assemblages of submarine landforms in the glacial troughs of the northern Barents Sea, east of Svalbard |
title_sort |
assemblages of submarine landforms in the glacial troughs of the northern barents sea, east of svalbard |
publisher |
Geological Society of London |
publishDate |
2016 |
url |
http://nora.nerc.ac.uk/id/eprint/515711/ https://doi.org/10.1144/M46.170 |
geographic |
Svalbard Barents Sea |
geographic_facet |
Svalbard Barents Sea |
genre |
Barents Sea Ice Sheet Sea ice Svalbard |
genre_facet |
Barents Sea Ice Sheet Sea ice Svalbard |
op_relation |
Hogan, Kelly A. orcid:0000-0002-1256-8010 Dowdeswell, J. A.; Noormets, R. 2016 Assemblages of submarine landforms in the glacial troughs of the northern Barents Sea, east of Svalbard. In: Dowdeswell, J.A.; Canals, M.; Jakobsson, M.; Todd, B.J.; Dowdeswell, E.K.; Hogan, K.A. orcid:0000-0002-1256-8010 , (eds.) Atlas of submarine glacial landforms: modern, Quaternary and ancient. London, Geological Society of London, 333-336. (Geological Society Memoir, 46, 46). |
op_doi |
https://doi.org/10.1144/M46.170 |
container_title |
Geological Society, London, Memoirs |
container_volume |
46 |
container_issue |
1 |
container_start_page |
333 |
op_container_end_page |
336 |
_version_ |
1766368782656208896 |