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Autor:
Eivind Sønstegaard, John Inge Svendsen, Anna L.C. Hughes, Inge Aarseth, Jan Mangerud, Kåre Skår, Øystein S. Lohne
Publikováno v:
Quaternary Science Reviews. 132:175-205
Distinct Younger Dryas (YD) moraines are mapped more-or-less continuously around the Scandinavian Ice Sheet. In most areas there is no evidence to suggest that a glacial re-advance took place during the YD, either because it did not happen or because