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 |
|---|---|
| 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