The maximum extent of glaciers in part of West Falkland
Abstract Although it is known that cirque glaciers once existed in the Falkland Islands, it has remained in doubt whether or not the islands were ever covered by ice caps or an ice sheet during the Cainozoic. This paper scrutinizes geomorphological evigernce on the south-eastern flank of a high mass...
Published in: | Journal of Glaciology |
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Language: | English |
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Cambridge University Press (CUP)
1976
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Online Access: | http://dx.doi.org/10.1017/s0022143000030732 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000030732 |
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crcambridgeupr:10.1017/s0022143000030732 2024-03-03T08:45:25+00:00 The maximum extent of glaciers in part of West Falkland Clapperton, C. M. Suggern, D. E. 1976 http://dx.doi.org/10.1017/s0022143000030732 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000030732 en eng Cambridge University Press (CUP) Journal of Glaciology volume 17, issue 75, page 73-77 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1976 crcambridgeupr https://doi.org/10.1017/s0022143000030732 2024-02-08T08:37:11Z Abstract Although it is known that cirque glaciers once existed in the Falkland Islands, it has remained in doubt whether or not the islands were ever covered by ice caps or an ice sheet during the Cainozoic. This paper scrutinizes geomorphological evigernce on the south-eastern flank of a high massif in West Falkland. It is suggested that, at the time of their maximum extent in the Cainozoic, the largest glaciers were no more than 2.7 km long. Article in Journal/Newspaper Ice Sheet Journal of Glaciology Cambridge University Press Journal of Glaciology 17 75 73 77 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
Earth-Surface Processes |
spellingShingle |
Earth-Surface Processes Clapperton, C. M. Suggern, D. E. The maximum extent of glaciers in part of West Falkland |
topic_facet |
Earth-Surface Processes |
description |
Abstract Although it is known that cirque glaciers once existed in the Falkland Islands, it has remained in doubt whether or not the islands were ever covered by ice caps or an ice sheet during the Cainozoic. This paper scrutinizes geomorphological evigernce on the south-eastern flank of a high massif in West Falkland. It is suggested that, at the time of their maximum extent in the Cainozoic, the largest glaciers were no more than 2.7 km long. |
format |
Article in Journal/Newspaper |
author |
Clapperton, C. M. Suggern, D. E. |
author_facet |
Clapperton, C. M. Suggern, D. E. |
author_sort |
Clapperton, C. M. |
title |
The maximum extent of glaciers in part of West Falkland |
title_short |
The maximum extent of glaciers in part of West Falkland |
title_full |
The maximum extent of glaciers in part of West Falkland |
title_fullStr |
The maximum extent of glaciers in part of West Falkland |
title_full_unstemmed |
The maximum extent of glaciers in part of West Falkland |
title_sort |
maximum extent of glaciers in part of west falkland |
publisher |
Cambridge University Press (CUP) |
publishDate |
1976 |
url |
http://dx.doi.org/10.1017/s0022143000030732 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000030732 |
genre |
Ice Sheet Journal of Glaciology |
genre_facet |
Ice Sheet Journal of Glaciology |
op_source |
Journal of Glaciology volume 17, issue 75, page 73-77 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000030732 |
container_title |
Journal of Glaciology |
container_volume |
17 |
container_issue |
75 |
container_start_page |
73 |
op_container_end_page |
77 |
_version_ |
1792500975082143744 |