Geomorphology and glacial history of Rauer Group, East Antarctica
The presence of glacial sediments across the Rauer Group indicates that the East Antarctic ice sheet formerly covered the entire archipelago and has since retreated at least 15 km from its maximum extent. The degree of weathering of these glacial sediments suggests that ice retreat from this maximum...
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Elsevier Inc.
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ftunivtasecite:oai:ecite.utas.edu.au:57959 2023-05-15T13:35:38+02:00 Geomorphology and glacial history of Rauer Group, East Antarctica White, DA Bennike, O Berg, S Harley, SL Fink, D Kiernan, K McConnell, A Wagner, B 2009 application/pdf http://www.sciencedirect.com https://doi.org/10.1016/j.yqres.2009.04.001 http://ecite.utas.edu.au/57959 en eng Elsevier Inc. http://ecite.utas.edu.au/57959/1/White DA.pdf http://dx.doi.org/10.1016/j.yqres.2009.04.001 White, DA and Bennike, O and Berg, S and Harley, SL and Fink, D and Kiernan, K and McConnell, A and Wagner, B, Geomorphology and glacial history of Rauer Group, East Antarctica, Quaternary Research, 72, (1) pp. 80-90. ISSN 0033-5894 (2009) [Refereed Article] http://ecite.utas.edu.au/57959 Earth Sciences Physical Geography and Environmental Geoscience Geomorphology and Regolith and Landscape Evolution Refereed Article PeerReviewed 2009 ftunivtasecite https://doi.org/10.1016/j.yqres.2009.04.001 2019-12-13T21:29:39Z The presence of glacial sediments across the Rauer Group indicates that the East Antarctic ice sheet formerly covered the entire archipelago and has since retreated at least 15 km from its maximum extent. The degree of weathering of these glacial sediments suggests that ice retreat from this maximum position occurred sometime during the latter half of the last glacial cycle. Following this phase of retreat, the ice sheet margin has not expanded more than 1 km seaward of its present position. This pattern of ice sheet change matches that recorded in Vestfold Hills, providing further evidence that the diminutive Marine Isotope Stage 2 ice sheet advance in the nearby Larsemann Hills may have been influenced by local factors rather than a regional ice-sheet response to climate and sea-level change. Article in Journal/Newspaper Antarc* Antarctic Antarctica East Antarctica Ice Sheet eCite UTAS (University of Tasmania) Antarctic East Antarctic Ice Sheet East Antarctica Larsemann Hills ENVELOPE(76.217,76.217,-69.400,-69.400) Rauer Group ENVELOPE(77.833,77.833,-68.850,-68.850) Vestfold Vestfold Hills Quaternary Research 72 1 80 90 |
institution |
Open Polar |
collection |
eCite UTAS (University of Tasmania) |
op_collection_id |
ftunivtasecite |
language |
English |
topic |
Earth Sciences Physical Geography and Environmental Geoscience Geomorphology and Regolith and Landscape Evolution |
spellingShingle |
Earth Sciences Physical Geography and Environmental Geoscience Geomorphology and Regolith and Landscape Evolution White, DA Bennike, O Berg, S Harley, SL Fink, D Kiernan, K McConnell, A Wagner, B Geomorphology and glacial history of Rauer Group, East Antarctica |
topic_facet |
Earth Sciences Physical Geography and Environmental Geoscience Geomorphology and Regolith and Landscape Evolution |
description |
The presence of glacial sediments across the Rauer Group indicates that the East Antarctic ice sheet formerly covered the entire archipelago and has since retreated at least 15 km from its maximum extent. The degree of weathering of these glacial sediments suggests that ice retreat from this maximum position occurred sometime during the latter half of the last glacial cycle. Following this phase of retreat, the ice sheet margin has not expanded more than 1 km seaward of its present position. This pattern of ice sheet change matches that recorded in Vestfold Hills, providing further evidence that the diminutive Marine Isotope Stage 2 ice sheet advance in the nearby Larsemann Hills may have been influenced by local factors rather than a regional ice-sheet response to climate and sea-level change. |
format |
Article in Journal/Newspaper |
author |
White, DA Bennike, O Berg, S Harley, SL Fink, D Kiernan, K McConnell, A Wagner, B |
author_facet |
White, DA Bennike, O Berg, S Harley, SL Fink, D Kiernan, K McConnell, A Wagner, B |
author_sort |
White, DA |
title |
Geomorphology and glacial history of Rauer Group, East Antarctica |
title_short |
Geomorphology and glacial history of Rauer Group, East Antarctica |
title_full |
Geomorphology and glacial history of Rauer Group, East Antarctica |
title_fullStr |
Geomorphology and glacial history of Rauer Group, East Antarctica |
title_full_unstemmed |
Geomorphology and glacial history of Rauer Group, East Antarctica |
title_sort |
geomorphology and glacial history of rauer group, east antarctica |
publisher |
Elsevier Inc. |
publishDate |
2009 |
url |
http://www.sciencedirect.com https://doi.org/10.1016/j.yqres.2009.04.001 http://ecite.utas.edu.au/57959 |
long_lat |
ENVELOPE(76.217,76.217,-69.400,-69.400) ENVELOPE(77.833,77.833,-68.850,-68.850) |
geographic |
Antarctic East Antarctic Ice Sheet East Antarctica Larsemann Hills Rauer Group Vestfold Vestfold Hills |
geographic_facet |
Antarctic East Antarctic Ice Sheet East Antarctica Larsemann Hills Rauer Group Vestfold Vestfold Hills |
genre |
Antarc* Antarctic Antarctica East Antarctica Ice Sheet |
genre_facet |
Antarc* Antarctic Antarctica East Antarctica Ice Sheet |
op_relation |
http://ecite.utas.edu.au/57959/1/White DA.pdf http://dx.doi.org/10.1016/j.yqres.2009.04.001 White, DA and Bennike, O and Berg, S and Harley, SL and Fink, D and Kiernan, K and McConnell, A and Wagner, B, Geomorphology and glacial history of Rauer Group, East Antarctica, Quaternary Research, 72, (1) pp. 80-90. ISSN 0033-5894 (2009) [Refereed Article] http://ecite.utas.edu.au/57959 |
op_doi |
https://doi.org/10.1016/j.yqres.2009.04.001 |
container_title |
Quaternary Research |
container_volume |
72 |
container_issue |
1 |
container_start_page |
80 |
op_container_end_page |
90 |
_version_ |
1766068144033497088 |