Glacial and periglacial phenomena in Ethiopia: a review
Stefan Grab
Permafrost and Periglacial Processes, 2002, vol. 13, issue 1, 71-76
Abstract:
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.
Date: 2002
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https://doi.org/10.1002/ppp.405
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Persistent link: https://EconPapers.repec.org/RePEc:wly:perpro:v:13:y:2002:i:1:p:71-76
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