Environmental controls on sediment composition and particle fluxes over the Antarctic continental shelf
14 pages, 7 figures The Antarctic continental shelf, covering approximately 4 • 106km2, has unique morphologic andtopographic characteristics shaped by its polar climate setting (Jacobs, 1989; Anderson and Thomas, 1991). The isostatic depression of the Antarctic continent by the ice sheet over it an...
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ftcsic:oai:digital.csic.es:10261/135138 2024-02-11T09:57:56+01:00 Environmental controls on sediment composition and particle fluxes over the Antarctic continental shelf Isla, Enrique 2016 http://hdl.handle.net/10261/135138 https://doi.org/10.1017/CBO9781107705791.017 unknown Cambridge University Press https://doi.org/10.1017/CBO9781107705791.017 Sí isbn: 9781107068223 Source-to-Sink Fluxes in Undisturbed Cold Environments 16: 199-212 (2016) http://hdl.handle.net/10261/135138 doi:10.1017/CBO9781107705791.017 none capítulo de libro http://purl.org/coar/resource_type/c_3248 2016 ftcsic https://doi.org/10.1017/CBO9781107705791.017 2024-01-16T10:16:38Z 14 pages, 7 figures The Antarctic continental shelf, covering approximately 4 • 106km2, has unique morphologic andtopographic characteristics shaped by its polar climate setting (Jacobs, 1989; Anderson and Thomas, 1991). The isostatic depression of the Antarctic continent by the ice sheet over it and the erosive glacial advance toward the sea has made the surrounding continental shelf broader and deeper than elsewhere. On average it has 500 m depth, whereas in the rest of the world it is 130 m depth; in some regions of West Antarctica this oceanic province can be up to 300 km wide such as in the western Weddell Sea, whereas the eastern section averages 100 km between 60ºE and 170ºE and about 60 km between 60ºE and 35ºW (Anderson, 1991, 1999). Typically, the continental shelf shows a fore deepened cross-shelf profile where the shallowest point is on the shelf break with water depths commonly exceeding 1,000 m on the inner shelf as a consequence of the aforementioned glacial processes (Anderson and Thomas, 1991) Peer Reviewed Book Part Antarc* Antarctic Antarctica Ice Sheet Weddell Sea West Antarctica Digital.CSIC (Spanish National Research Council) Antarctic The Antarctic Weddell Weddell Sea West Antarctica 199 212 |
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Digital.CSIC (Spanish National Research Council) |
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14 pages, 7 figures The Antarctic continental shelf, covering approximately 4 • 106km2, has unique morphologic andtopographic characteristics shaped by its polar climate setting (Jacobs, 1989; Anderson and Thomas, 1991). The isostatic depression of the Antarctic continent by the ice sheet over it and the erosive glacial advance toward the sea has made the surrounding continental shelf broader and deeper than elsewhere. On average it has 500 m depth, whereas in the rest of the world it is 130 m depth; in some regions of West Antarctica this oceanic province can be up to 300 km wide such as in the western Weddell Sea, whereas the eastern section averages 100 km between 60ºE and 170ºE and about 60 km between 60ºE and 35ºW (Anderson, 1991, 1999). Typically, the continental shelf shows a fore deepened cross-shelf profile where the shallowest point is on the shelf break with water depths commonly exceeding 1,000 m on the inner shelf as a consequence of the aforementioned glacial processes (Anderson and Thomas, 1991) Peer Reviewed |
format |
Book Part |
author |
Isla, Enrique |
spellingShingle |
Isla, Enrique Environmental controls on sediment composition and particle fluxes over the Antarctic continental shelf |
author_facet |
Isla, Enrique |
author_sort |
Isla, Enrique |
title |
Environmental controls on sediment composition and particle fluxes over the Antarctic continental shelf |
title_short |
Environmental controls on sediment composition and particle fluxes over the Antarctic continental shelf |
title_full |
Environmental controls on sediment composition and particle fluxes over the Antarctic continental shelf |
title_fullStr |
Environmental controls on sediment composition and particle fluxes over the Antarctic continental shelf |
title_full_unstemmed |
Environmental controls on sediment composition and particle fluxes over the Antarctic continental shelf |
title_sort |
environmental controls on sediment composition and particle fluxes over the antarctic continental shelf |
publisher |
Cambridge University Press |
publishDate |
2016 |
url |
http://hdl.handle.net/10261/135138 https://doi.org/10.1017/CBO9781107705791.017 |
geographic |
Antarctic The Antarctic Weddell Weddell Sea West Antarctica |
geographic_facet |
Antarctic The Antarctic Weddell Weddell Sea West Antarctica |
genre |
Antarc* Antarctic Antarctica Ice Sheet Weddell Sea West Antarctica |
genre_facet |
Antarc* Antarctic Antarctica Ice Sheet Weddell Sea West Antarctica |
op_relation |
https://doi.org/10.1017/CBO9781107705791.017 Sí isbn: 9781107068223 Source-to-Sink Fluxes in Undisturbed Cold Environments 16: 199-212 (2016) http://hdl.handle.net/10261/135138 doi:10.1017/CBO9781107705791.017 |
op_rights |
none |
op_doi |
https://doi.org/10.1017/CBO9781107705791.017 |
container_start_page |
199 |
op_container_end_page |
212 |
_version_ |
1790593473699643392 |