EconPapers    
Economics at your fingertips  
 

The occurrence of a holocene rock glacier on Mount Kenya: Some observations and comments

Stefan W. Grab

Permafrost and Periglacial Processes, 1996, vol. 7, issue 4, 381-389

Abstract: The morphology of the Lenana rock glacier is briefly described from Mount Kenya. Biological activity and ground temperature data do not support contemporary rock glacier development at the site. It is suggested that the rock glacier and protalus ramparts were active during the Holocene and are indicative of a recent frozen core and perennial snowbanks above ∼4750 m ASL. © 1996 John Wiley & Sons, Ltd.

Date: 1996
References: Add references at CitEc
Citations:

Downloads: (external link)
https://doi.org/10.1002/(SICI)1099-1530(199610)7:43.0.CO;2-5

Related works:
This item may be available elsewhere in EconPapers: Search for items with the same title.

Export reference: BibTeX RIS (EndNote, ProCite, RefMan) HTML/Text

Persistent link: https://EconPapers.repec.org/RePEc:wly:perpro:v:7:y:1996:i:4:p:381-389

Access Statistics for this article

More articles in Permafrost and Periglacial Processes from John Wiley & Sons
Bibliographic data for series maintained by Wiley Content Delivery ().

 
Page updated 2025-03-20
Handle: RePEc:wly:perpro:v:7:y:1996:i:4:p:381-389