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...

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Published in:Journal of Glaciology
Main Authors: Clapperton, C. M., Suggern, D. E.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1976
Subjects:
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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spelling 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
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