Abstract
Present-day processes in this badland are described and the geomorphological environment of prehistoric time is reconstructed. Most of the erosion is post-Mousterian. There have been at least two erosive phases and one depositional phase in the last 80 000 years. The severe erosion is attributed to a past period with heavier rainfall events. -Keith Clayton
| Original language | English |
|---|---|
| Pages (from-to) | 125-135 |
| Number of pages | 11 |
| Journal | Sahara and surrounding sea; sediments and climatic changes, Proc. symposium, Mainz, 1979 |
| State | Published - 1980 |
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