The AA. hypothesize that 1) many of the subhorizontally stratified deposits represent full-glacial eolian sand sheets, formed when sand supply was limited by seasonally variable combinations of ice cementation, snow cover, high groundwater tables
Geological and geomorphological investigations, carried through by the authors to the south and the north of Hornsund, supplied with new data on Würm and Holocene glaciations in this part of Spitsbergen. Most information from that came from