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  • Geologic and geomorphologic research in the Lisbet Valley and Kulmstranda proved a glaciation of the southern coast of Hornsund during the Würm/Vistulian/Glaciation. Maximum of this glaciation, expressed by an advance of glaciers in Hornsund
  • the Valleys: Slaklidalen and Revdalen. It proved that the Hornsund region was completely covered by the Würm glaciers about 45-40 thousand years BP. The following Würm glacier advances occupied smaller areas. The glaciers probably contacted