Perennially frozen lakes at glacier/ rock margins, East Antarctica.
Perenially frozen lakes partially bounded by icesheet or glacier ice occur widely in Antarctica. Lakes form when meltwater at the rock margin becomes deeper than the winter freezing point. Thermo-erosion of glacier ice expands the lake, and as the glacier ice capping the lake ablates, it is replaced...
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ftmacquarieunicr:oai:https://researchers.mq.edu.au:publications/331bf4e1-ceb7-43d1-9210-1e3a576ba4df 2023-05-15T13:51:16+02:00 Perennially frozen lakes at glacier/ rock margins, East Antarctica. Pickard, J. Adamson, D. A. 1983 https://researchers.mq.edu.au/en/publications/331bf4e1-ceb7-43d1-9210-1e3a576ba4df http://www.scopus.com/inward/record.url?scp=0021027392&partnerID=8YFLogxK eng eng info:eu-repo/semantics/restrictedAccess Pickard , J & Adamson , D A 1983 , ' Perennially frozen lakes at glacier/ rock margins, East Antarctica. ' , American Society of Mechanical Engineers (Paper) , pp. 470-472 . article 1983 ftmacquarieunicr 2022-02-18T14:47:55Z Perenially frozen lakes partially bounded by icesheet or glacier ice occur widely in Antarctica. Lakes form when meltwater at the rock margin becomes deeper than the winter freezing point. Thermo-erosion of glacier ice expands the lake, and as the glacier ice capping the lake ablates, it is replaced from below by refrozen lake water. Diapiric domes occur on smaller lakes, and pressure ridges on large lakes. Debris deposits on nunatak slopes above lakes include lacustrine sediments as well as scree and till. Strandlines of boulders indicate stages in icesheet lowering, while water marks on rock bluffs indicate stages in lowering of the lakes. -from Authors Article in Journal/Newspaper Antarc* Antarctica East Antarctica Macquarie University Research Portal East Antarctica |
institution |
Open Polar |
collection |
Macquarie University Research Portal |
op_collection_id |
ftmacquarieunicr |
language |
English |
description |
Perenially frozen lakes partially bounded by icesheet or glacier ice occur widely in Antarctica. Lakes form when meltwater at the rock margin becomes deeper than the winter freezing point. Thermo-erosion of glacier ice expands the lake, and as the glacier ice capping the lake ablates, it is replaced from below by refrozen lake water. Diapiric domes occur on smaller lakes, and pressure ridges on large lakes. Debris deposits on nunatak slopes above lakes include lacustrine sediments as well as scree and till. Strandlines of boulders indicate stages in icesheet lowering, while water marks on rock bluffs indicate stages in lowering of the lakes. -from Authors |
format |
Article in Journal/Newspaper |
author |
Pickard, J. Adamson, D. A. |
spellingShingle |
Pickard, J. Adamson, D. A. Perennially frozen lakes at glacier/ rock margins, East Antarctica. |
author_facet |
Pickard, J. Adamson, D. A. |
author_sort |
Pickard, J. |
title |
Perennially frozen lakes at glacier/ rock margins, East Antarctica. |
title_short |
Perennially frozen lakes at glacier/ rock margins, East Antarctica. |
title_full |
Perennially frozen lakes at glacier/ rock margins, East Antarctica. |
title_fullStr |
Perennially frozen lakes at glacier/ rock margins, East Antarctica. |
title_full_unstemmed |
Perennially frozen lakes at glacier/ rock margins, East Antarctica. |
title_sort |
perennially frozen lakes at glacier/ rock margins, east antarctica. |
publishDate |
1983 |
url |
https://researchers.mq.edu.au/en/publications/331bf4e1-ceb7-43d1-9210-1e3a576ba4df http://www.scopus.com/inward/record.url?scp=0021027392&partnerID=8YFLogxK |
geographic |
East Antarctica |
geographic_facet |
East Antarctica |
genre |
Antarc* Antarctica East Antarctica |
genre_facet |
Antarc* Antarctica East Antarctica |
op_source |
Pickard , J & Adamson , D A 1983 , ' Perennially frozen lakes at glacier/ rock margins, East Antarctica. ' , American Society of Mechanical Engineers (Paper) , pp. 470-472 . |
op_rights |
info:eu-repo/semantics/restrictedAccess |
_version_ |
1766255034201276416 |