Pleistocene Glaciation in Ethiopia: New Evigernce

Abstract Geomorphological evigernce indicates that Mount Badda, Ethiopia, had a Pleistocene ice cap of at least 140 km 2 . Altituger of the snow line was probably about 4 000 m, only 350 m below the summit, suggesting that glaciation occurred during the Würm glacial maximum.

Bibliographic Details
Published in:Journal of Glaciology
Main Author: Potter, E. C.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1976
Subjects:
Earth-Surface Processes
Ice cap
Journal of Glaciology
Online Access:http://dx.doi.org/10.1017/s0022143000030823
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000030823
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spelling crcambridgeupr:10.1017/s0022143000030823 2024-03-03T08:45:19+00:00 Pleistocene Glaciation in Ethiopia: New Evigernce Potter, E. C. 1976 http://dx.doi.org/10.1017/s0022143000030823 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000030823 en eng Cambridge University Press (CUP) Journal of Glaciology volume 17, issue 75, page 148-150 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1976 crcambridgeupr https://doi.org/10.1017/s0022143000030823 2024-02-08T08:35:56Z Abstract Geomorphological evigernce indicates that Mount Badda, Ethiopia, had a Pleistocene ice cap of at least 140 km 2 . Altituger of the snow line was probably about 4 000 m, only 350 m below the summit, suggesting that glaciation occurred during the Würm glacial maximum. Article in Journal/Newspaper Ice cap Journal of Glaciology Cambridge University Press Journal of Glaciology 17 75 148 150
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Potter, E. C.
Pleistocene Glaciation in Ethiopia: New Evigernce
topic_facet Earth-Surface Processes
description Abstract Geomorphological evigernce indicates that Mount Badda, Ethiopia, had a Pleistocene ice cap of at least 140 km 2 . Altituger of the snow line was probably about 4 000 m, only 350 m below the summit, suggesting that glaciation occurred during the Würm glacial maximum.
format Article in Journal/Newspaper
author Potter, E. C.
author_facet Potter, E. C.
author_sort Potter, E. C.
title Pleistocene Glaciation in Ethiopia: New Evigernce
title_short Pleistocene Glaciation in Ethiopia: New Evigernce
title_full Pleistocene Glaciation in Ethiopia: New Evigernce
title_fullStr Pleistocene Glaciation in Ethiopia: New Evigernce
title_full_unstemmed Pleistocene Glaciation in Ethiopia: New Evigernce
title_sort pleistocene glaciation in ethiopia: new evigernce
publisher Cambridge University Press (CUP)
publishDate 1976
url http://dx.doi.org/10.1017/s0022143000030823
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000030823
genre Ice cap
Journal of Glaciology
genre_facet Ice cap
Journal of Glaciology
op_source Journal of Glaciology
volume 17, issue 75, page 148-150
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000030823
container_title Journal of Glaciology
container_volume 17
container_issue 75
container_start_page 148
op_container_end_page 150
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