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  • The author shows the history of the Carpathian geological vertical zones during the Late Pleistocene and Early Holocene. The warming of climate, from a continental periglacial climate to a more oceanic one, and the rise in humidity were two engines
  • 1992
  • Geological history of the upper Vistula starting from formation of the Carpathian foredeep and Cracow gate through the Quaternary, followed by the human impact of the Neolithic farmers, Iron age industry and historical period. Special attention
  • 1992