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 |
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Pages (from-to) | 125-135 |
Number of pages | 11 |
Journal | Unknown Journal |
State | Published - 1980 |