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Publication Details
AFRICAN RESEARCH NEXUS
SHINING A SPOTLIGHT ON AFRICAN RESEARCH
Observations on a blockstream in the vicinity of Sani Pass, Lesotho highlands, southern Africa
Permafrost and Periglacial Processes, Volume 13, No. 4, Year 2002
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Description
Coarse slope deposits, frequently grading into blockstreams, are common throughout the Lesotho highlands, southern Africa. This paper describes one such blockstream. It is interpreted as a typical lag deposit derived from valley-wide colluvial mantles, which contains superimposed and incorporated Late-Pleistocene blocky material. Blocks are largely derived from local scarps but may contain a component of corestones from mobilized regolith. The widespread mantle argues against landscape-scale glaciation in the Lesotho highlands in the Late Pleistocene. Rather, the environment appears to have been conducive to deep seasonal frost during the period of block production. No unequivocal evidence for permafrost is found. Copyright © 2002 John Wiley and Sons, Ltd.
Authors & Co-Authors
Boelhouwers, Jan C.
Sweden, Uppsala
Uppsala Universitet
Holness, Stephen Dale
South Africa, Bellville
University of the Western Cape
Meiklejohn, Ian
South Africa, Pretoria
University of Pretoria
Sumner, Paul Douglas
South Africa, Pretoria
University of Pretoria
Statistics
Citations: 47
Authors: 4
Affiliations: 3
Identifiers
Doi:
10.1002/ppp.428
Study Locations
Lesotho