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  • 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
  • with the Scandinavian ice sheet of that time through the Barents Shelf ice sheet. The following glacier advances in the described area occurred about 11-10 thousand years BP and in Late Holocene: at 2.5-2 thousand years BP and during Ice Age. (AA).