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  • . The last major period of calcrete formation probably took place at least 14 000 years BP, under a climate drier than the present, between the close of the Middle Stone Age and the last major aeolian redistribution of the sands of Kalahari type
  • Glacial age aeolian events at high and low latitudes: a Southern Hemisphere perspective in Antarctic glacial history and world palaeoenvironments.
  • questions. The analysis yielded results that question assumptions that the limestone surface has undergone deformation and is multicyclic. It confirms the view that in the Namib there exist two limestones capable of hosting karst that are age and altitude