Abstract
Abstract The Scandinavian Ice Sheet formed around 12.6 Ma and expanded considerably from 2.7 Ma. During the Weichselian the western margin reached the coast during Marine Isotope Stage (MIS) 5d and the continental shelf during MIS 5b, MIS 4 and MIS 2. It was almost gone during MIS 5c and 5a, and was much reduced during periods of MIS 3, notably the Alesund interstadial. There was a re-advance during the Younger Dryas.
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