Glacial and periglacial phenomena in Ethiopia: a review

The glacial and periglacial geomorphology for the Simen and Bale Mountains in Ethiopia is reviewed. The Simen Mountains are mostly absent of relict periglacial landforms and today host a variety of miniature cryogenic phenomena. The Bale Mountains host a few localized large relict cryogenic landform...

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Published in:Permafrost and Periglacial Processes
Main Author: Stefan Grab
Format: Article in Journal/Newspaper
Language:unknown
Subjects:
Online Access:https://doi.org/10.1002/ppp.405
id ftrepec:oai:RePEc:wly:perpro:v:13:y:2002:i:1:p:71-76
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spelling ftrepec:oai:RePEc:wly:perpro:v:13:y:2002:i:1:p:71-76 2023-05-15T17:57:23+02:00 Glacial and periglacial phenomena in Ethiopia: a review Stefan Grab https://doi.org/10.1002/ppp.405 unknown https://doi.org/10.1002/ppp.405 article ftrepec https://doi.org/10.1002/ppp.405 2020-12-04T13:31:25Z The glacial and periglacial geomorphology for the Simen and Bale Mountains in Ethiopia is reviewed. The Simen Mountains are mostly absent of relict periglacial landforms and today host a variety of miniature cryogenic phenomena. The Bale Mountains host a few localized large relict cryogenic landforms (e.g. stone stripes), suggesting past sporadic permafrost. A variety of regional factors may have contributed to the more extensive periglacial activity in southern Ethiopia than in the higher Simen Mountains to the north. Copyright © 2002 John Wiley & Sons, Ltd. Article in Journal/Newspaper permafrost RePEc (Research Papers in Economics) Permafrost and Periglacial Processes 13 1 71 76
institution Open Polar
collection RePEc (Research Papers in Economics)
op_collection_id ftrepec
language unknown
description The glacial and periglacial geomorphology for the Simen and Bale Mountains in Ethiopia is reviewed. The Simen Mountains are mostly absent of relict periglacial landforms and today host a variety of miniature cryogenic phenomena. The Bale Mountains host a few localized large relict cryogenic landforms (e.g. stone stripes), suggesting past sporadic permafrost. A variety of regional factors may have contributed to the more extensive periglacial activity in southern Ethiopia than in the higher Simen Mountains to the north. Copyright © 2002 John Wiley & Sons, Ltd.
format Article in Journal/Newspaper
author Stefan Grab
spellingShingle Stefan Grab
Glacial and periglacial phenomena in Ethiopia: a review
author_facet Stefan Grab
author_sort Stefan Grab
title Glacial and periglacial phenomena in Ethiopia: a review
title_short Glacial and periglacial phenomena in Ethiopia: a review
title_full Glacial and periglacial phenomena in Ethiopia: a review
title_fullStr Glacial and periglacial phenomena in Ethiopia: a review
title_full_unstemmed Glacial and periglacial phenomena in Ethiopia: a review
title_sort glacial and periglacial phenomena in ethiopia: a review
url https://doi.org/10.1002/ppp.405
genre permafrost
genre_facet permafrost
op_relation https://doi.org/10.1002/ppp.405
op_doi https://doi.org/10.1002/ppp.405
container_title Permafrost and Periglacial Processes
container_volume 13
container_issue 1
container_start_page 71
op_container_end_page 76
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