Abstract
The elevation of the pavement and the presence of dark-grey Karoo shales in minor valleys along the flank of the large Permo-Carboniferous Kaap Valley imply that the Ghaap Escarpment was a pre-glacial topographic feature and that palaeoice flow was entirely controlled by the topographic grain of the region.-from Authors
Original language | English |
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Pages (from-to) | 385-388 |
Number of pages | 4 |
Journal | Transactions - Geological Society of South Africa |
Volume | 89 |
Issue number | 3 |
Publication status | Published - 1986 |
Externally published | Yes |
ASJC Scopus subject areas
- General Environmental Science
- General Engineering
- General Earth and Planetary Sciences