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  • and mineralogical analysis of soils and sdiments and were supplemented by TL-dating of selected samples. The use of different methods allows a better understanding of landform development in the southwestern Kalahari as well as attempts of a paleoclimatic
  • 1997
  • ; deflation-moderating impact of irrigation varied in extent with 27 different soil samples. The experiments are capable of providing useful data for the initial stage of form development in wind-blown sand areas, as well.
  • 1997
  • Inactivated aeolian sediments and forms allow of conclusions on former processes of environmental development in arid zones, though only in comparison with additional morphological, pedological, and palynological findings. This correlation
  • 1997