GEOMORPHIC EVOLUTION OF DEBRIS FANS IN THE DU TOIT'S KLOOF, WESTERN CAPE MOUNTAINS
Author:
Affiliation:
1. a Department of Earth Sciences , Uppsala University , Villavägen 16, 752 36 , Uppsala , Sweden E-mail:
2. b Department of Physical Geography , Utrecht University , P.O.Box 80.115, 3508 , TC , Utrecht , The Netherlands
Publisher
Informa UK Limited
Subject
General Earth and Planetary Sciences,Geography, Planning and Development
Link
https://www.tandfonline.com/doi/pdf/10.1080/03736245.2001.9713745
Reference21 articles.
1. AGROMET. 1992. Climatic statistics for the winter rainfall region, 108ppElsenburg: Institute for Soil, Water and Climate.
2. Holocene geomorphic activity in the Scottish Highlands
3. Rockfall Activity in Upland Britain during the Loch Lomond Stadial
4. A Discussion Regarding Weathering in the Western Cape Mountains, South Africa: Implications for Pleistocene Cryoclastic Debris Production
5. Boelhouwers, J. C. 1998. The Present-Day Frost Action Environments and its Geomorphological Significance in the Western Cape Mountains, South Africa, 179ppBellville: School of Environmental Studies, University of the Western Cape. Occasional Publication Series, 2
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