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  • The A. gives a review of oceanic areas of the world, which obtain increasing importance concerning in the development of geological sciences with regard to the basic geological research as well as to the applied geological research, especially
  • 1983
  • Hurricanes, storms and tornadoes: geographic characteristics and geologic activity.
  • 1983
  • The distributions and affinities of the macrolepidopteran taxa known from south-eastern Polynesia are investigated and contrasted with various geological hypotheses for the origin of the islands. A colonialist interpretation, long distance dispersal
  • 1983
  • is based on gravity, magnetic and geological data, and confirms the recently published geological schemes of this area thus amphasizing the importance of geophysical region division. Results of deep seismic soundings in the same area are discussed
  • 1983
  • Based on selected investigations, carried out in sulphate karst, ways to quantitive engeneering-geological results are pointed out. Such investigations always go back to comprehensive geological survey combined with geodetic work. Findings of other
  • 1983
  • Contributions on geological development of molasses in some regions of Europe and USSR and on block tectonics of Elbe-lineament
  • 1983
  • Current methods in biogeography are briefly reviewed and definitions of dispersal discussed. The need for countenancing the possibilities of operation of both the vicariance and dispersal modes is stressed, and for taking into account geological
  • 1983
  • The balance of soil moisture is concerned in connection with the flow of possibly toxic materials. The opportunities for the geostatical interpretation of geological, pedological and topographic maps are studied. For the handling of data a computer
  • 1983
  • Nowadays any investigation of recent marine sediments is carried out with pore water analysis. Their results contribute considerably to the solution of diagenetic and deposite-formation processes of the geological past. (HL).
  • 1983
  • slopes is closely related to the geological succession and structure. Examples of geomorphological maps, slope categories maps and cross sections are presented. It is suggested that whole-slope failures in this region have a maximum frequency of once
  • 1983