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  • diamicton. The age of the features is not known but they probably formed during the later part of the last Midlandian Glaciation when the plateau was ice-free.
  • and eroded materials deposited prior to 0.25-0.29 MY. The second generation is related to terraced alluvial sediments| both deposits are strongly weathered to form a fersiallitic soil of Eemian age. This soil contains artifacts of the final Acheulean