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  • . The mineralogical nature of a newly formed product depends mainly on the intensity of the leaching to which the profile is subjected, which is influenced by the rainfall in the area where they are found, as well as the size of existing voids in the material.
  • 1999
  • for glaciolacustrine varve sedimentation in the Baltic Ice Lake and the possibilities of making a detailed facies classification of the sediments in an area with an established varve chronology.
  • 1999
  • The nature of alternating layers of clayey soil material and calcareous soil material in the desert fringe area , (archaeological site at Revadim) is discussed. In earlier work, these soil materials were considered as representing different climatic
  • 1999
  • The terrestrial ice limits of the Last Glacial Maximum ice sheets are well understood, but areas submerged during postglacial sea level rise have proved more difficult to accurately map. Fine grained diamicts in the Southern North Sea have been
  • 1999