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Glacial and periglacial phenomena in Ethiopia: a review

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  • Stefan Grab

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.

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  • Stefan Grab, 2002. "Glacial and periglacial phenomena in Ethiopia: a review," Permafrost and Periglacial Processes, John Wiley & Sons, vol. 13(1), pages 71-76, March.
    • Handle: RePEc:wly:perpro:v:13:y:2002:i:1:p:71-76
    DOI: 10.1002/ppp.405
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