Protalus ramparts and the altitude of the local equilibrium line during the last glacial stage in Bokspruit, East Cape Drakensberg, South Africa
A ridge of unconsolidated debris at an altitude of 2000 m, located beneath cliffs in the East Cape Drakensberg of South Africa, is interpreted on morphological and sedimentological evidence as a protalus rampart. The rampart is believed to have formed in the Bottelnek Stadial, after 27 000 BP and be...
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| Format: | Article in Journal/Newspaper |
| Language: | English |
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1994
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| Online Access: | http://hdl.handle.net/10962/d1006729 https://corycommons.ru.ac.za/vital/access/manager/Repository/vital:6694 |