Former extension of the East Antarctic Ice Sheet
Knowledge about the Quarternary geology of the Australian sector of Antarctica is very incomplete. Scattered observations of glacial deposits in that area, made during the ANARE 6 expedition in 1987, indicate that the inland ice had formerly a considerably wider extension than today. The ice was mor...
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Norwegian Polar Institute
1989
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ftjpolarres:oai:journals.openacademia.net:article/2407 2023-05-15T14:01:21+02:00 Former extension of the East Antarctic Ice Sheet Lundqvist, Jan 1989-01-12 application/pdf https://polarresearch.net/index.php/polar/article/view/2407 https://doi.org/10.3402/polar.v7i2.6835 eng eng Norwegian Polar Institute https://polarresearch.net/index.php/polar/article/view/2407/5657 https://polarresearch.net/index.php/polar/article/view/2407 doi:10.3402/polar.v7i2.6835 Copyright (c) 2018 Polar Research Polar Research; Vol. 7 No. 2 (1989); 109-117 1751-8369 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 1989 ftjpolarres https://doi.org/10.3402/polar.v7i2.6835 2021-11-11T19:12:32Z Knowledge about the Quarternary geology of the Australian sector of Antarctica is very incomplete. Scattered observations of glacial deposits in that area, made during the ANARE 6 expedition in 1987, indicate that the inland ice had formerly a considerably wider extension than today. The ice was more than 200 m thicker, probably of the order 1, 000m. This maximum stage cannot yet be dated, but conditions seem to favour a late Wisconsin-Weichselian maximum age. However, a much higher age cannot be excluded. Article in Journal/Newspaper Antarc* Antarctic Antarctica Ice Sheet Polar Research Polar Research (E-Journal) Antarctic East Antarctic Ice Sheet Polar Research 7 2 109 117 |
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Open Polar |
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Polar Research (E-Journal) |
op_collection_id |
ftjpolarres |
language |
English |
description |
Knowledge about the Quarternary geology of the Australian sector of Antarctica is very incomplete. Scattered observations of glacial deposits in that area, made during the ANARE 6 expedition in 1987, indicate that the inland ice had formerly a considerably wider extension than today. The ice was more than 200 m thicker, probably of the order 1, 000m. This maximum stage cannot yet be dated, but conditions seem to favour a late Wisconsin-Weichselian maximum age. However, a much higher age cannot be excluded. |
format |
Article in Journal/Newspaper |
author |
Lundqvist, Jan |
spellingShingle |
Lundqvist, Jan Former extension of the East Antarctic Ice Sheet |
author_facet |
Lundqvist, Jan |
author_sort |
Lundqvist, Jan |
title |
Former extension of the East Antarctic Ice Sheet |
title_short |
Former extension of the East Antarctic Ice Sheet |
title_full |
Former extension of the East Antarctic Ice Sheet |
title_fullStr |
Former extension of the East Antarctic Ice Sheet |
title_full_unstemmed |
Former extension of the East Antarctic Ice Sheet |
title_sort |
former extension of the east antarctic ice sheet |
publisher |
Norwegian Polar Institute |
publishDate |
1989 |
url |
https://polarresearch.net/index.php/polar/article/view/2407 https://doi.org/10.3402/polar.v7i2.6835 |
geographic |
Antarctic East Antarctic Ice Sheet |
geographic_facet |
Antarctic East Antarctic Ice Sheet |
genre |
Antarc* Antarctic Antarctica Ice Sheet Polar Research |
genre_facet |
Antarc* Antarctic Antarctica Ice Sheet Polar Research |
op_source |
Polar Research; Vol. 7 No. 2 (1989); 109-117 1751-8369 |
op_relation |
https://polarresearch.net/index.php/polar/article/view/2407/5657 https://polarresearch.net/index.php/polar/article/view/2407 doi:10.3402/polar.v7i2.6835 |
op_rights |
Copyright (c) 2018 Polar Research |
op_doi |
https://doi.org/10.3402/polar.v7i2.6835 |
container_title |
Polar Research |
container_volume |
7 |
container_issue |
2 |
container_start_page |
109 |
op_container_end_page |
117 |
_version_ |
1766271083825070080 |