Meeresbodenmorphologie und glaziale Geschichte im Umfeld des Ekströmisen
Based on the results published in Ötting et al., 2022 (https://doi.org/10.5194/tc-16-2051-2022) we present a compilation of geophysical surveys in front of and beneath the Ekström Ice Shelf, to identify and interpret evidence of past ice-sheet flow, extent and retreat. The sea floor beneath the Ekst...
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ftawi:oai:epic.awi.de:56285 2023-05-15T16:41:20+02:00 Meeresbodenmorphologie und glaziale Geschichte im Umfeld des Ekströmisen Eisen, Olaf 2022-06-13 https://epic.awi.de/id/eprint/56285/ https://hdl.handle.net/10013/epic.c654e230-11a8-40cd-b796-c69394487db3 unknown Eisen, O. orcid:0000-0002-6380-962X (2022) Meeresbodenmorphologie und glaziale Geschichte im Umfeld des Ekströmisen , 17. Sitzung D-ANDRILL, AG des Nationalkomitees SCAR/IASC . hdl:10013/epic.c654e230-11a8-40cd-b796-c69394487db3 EPIC317. Sitzung D-ANDRILL, AG des Nationalkomitees SCAR/IASC Conference notRev 2022 ftawi 2022-10-09T23:12:45Z Based on the results published in Ötting et al., 2022 (https://doi.org/10.5194/tc-16-2051-2022) we present a compilation of geophysical surveys in front of and beneath the Ekström Ice Shelf, to identify and interpret evidence of past ice-sheet flow, extent and retreat. The sea floor beneath the Ekström Ice Shelf is dominated by an incised trough, which extends from the modern-day grounding line onto the continental shelf. Our surveys show that mega-scale glacial lineations cover most of the mouth of this trough, terminating 11 km away from the continental shelf break, indicating the most recent minimal extent of grounded ice in this region. Beneath the front ∼30 km of the ice shelf measured from the ice shelf edge towards the inland direction, the sea floor is characterised by an acoustically transparent sedimentary unit, up to 45 m thick. This is likely composed of subglacial till, further corroborating the presence of past grounded ice cover. Further inland, the sea floor becomes rougher, interpreted as a transition from subglacial tills to a crystalline bedrock, corresponding to the outcrop of the volcanic Explora Wedge at the sea floor. Ice retreat in this region appears to have happened rapidly in the centre of the incised trough, evidenced by a lack of overprinting of the lineations at the trough mouth. At the margins of the trough uniformly spaced recessional moraines suggest ice retreated more gradually. We estimate the palaeo-ice thickness at the calving front around the Last Glacial Maximum to have been at least 305 to 320 m, based on the depth of iceberg ploughmarks within the trough and sea level reconstructions. Conference Object Ice Sheet Ice Shelf Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) Ekström Ice Shelf ENVELOPE(-8.000,-8.000,-71.000,-71.000) Ekströmisen ENVELOPE(-8.000,-8.000,-71.000,-71.000) |
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Open Polar |
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Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |
op_collection_id |
ftawi |
language |
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description |
Based on the results published in Ötting et al., 2022 (https://doi.org/10.5194/tc-16-2051-2022) we present a compilation of geophysical surveys in front of and beneath the Ekström Ice Shelf, to identify and interpret evidence of past ice-sheet flow, extent and retreat. The sea floor beneath the Ekström Ice Shelf is dominated by an incised trough, which extends from the modern-day grounding line onto the continental shelf. Our surveys show that mega-scale glacial lineations cover most of the mouth of this trough, terminating 11 km away from the continental shelf break, indicating the most recent minimal extent of grounded ice in this region. Beneath the front ∼30 km of the ice shelf measured from the ice shelf edge towards the inland direction, the sea floor is characterised by an acoustically transparent sedimentary unit, up to 45 m thick. This is likely composed of subglacial till, further corroborating the presence of past grounded ice cover. Further inland, the sea floor becomes rougher, interpreted as a transition from subglacial tills to a crystalline bedrock, corresponding to the outcrop of the volcanic Explora Wedge at the sea floor. Ice retreat in this region appears to have happened rapidly in the centre of the incised trough, evidenced by a lack of overprinting of the lineations at the trough mouth. At the margins of the trough uniformly spaced recessional moraines suggest ice retreated more gradually. We estimate the palaeo-ice thickness at the calving front around the Last Glacial Maximum to have been at least 305 to 320 m, based on the depth of iceberg ploughmarks within the trough and sea level reconstructions. |
format |
Conference Object |
author |
Eisen, Olaf |
spellingShingle |
Eisen, Olaf Meeresbodenmorphologie und glaziale Geschichte im Umfeld des Ekströmisen |
author_facet |
Eisen, Olaf |
author_sort |
Eisen, Olaf |
title |
Meeresbodenmorphologie und glaziale Geschichte im Umfeld des Ekströmisen |
title_short |
Meeresbodenmorphologie und glaziale Geschichte im Umfeld des Ekströmisen |
title_full |
Meeresbodenmorphologie und glaziale Geschichte im Umfeld des Ekströmisen |
title_fullStr |
Meeresbodenmorphologie und glaziale Geschichte im Umfeld des Ekströmisen |
title_full_unstemmed |
Meeresbodenmorphologie und glaziale Geschichte im Umfeld des Ekströmisen |
title_sort |
meeresbodenmorphologie und glaziale geschichte im umfeld des ekströmisen |
publishDate |
2022 |
url |
https://epic.awi.de/id/eprint/56285/ https://hdl.handle.net/10013/epic.c654e230-11a8-40cd-b796-c69394487db3 |
long_lat |
ENVELOPE(-8.000,-8.000,-71.000,-71.000) ENVELOPE(-8.000,-8.000,-71.000,-71.000) |
geographic |
Ekström Ice Shelf Ekströmisen |
geographic_facet |
Ekström Ice Shelf Ekströmisen |
genre |
Ice Sheet Ice Shelf |
genre_facet |
Ice Sheet Ice Shelf |
op_source |
EPIC317. Sitzung D-ANDRILL, AG des Nationalkomitees SCAR/IASC |
op_relation |
Eisen, O. orcid:0000-0002-6380-962X (2022) Meeresbodenmorphologie und glaziale Geschichte im Umfeld des Ekströmisen , 17. Sitzung D-ANDRILL, AG des Nationalkomitees SCAR/IASC . hdl:10013/epic.c654e230-11a8-40cd-b796-c69394487db3 |
_version_ |
1766031762297716736 |