The Laurentide and Innuitian ice sheets during the Last Glacial Maximum
The Late Wisconsinan advance of the Laurentide Ice Sheet started from a Middle Wisconsinan interstadial minimum 27–30 14C ka BP when the ice margin approximately followed the boundary of the Canadian Shield. Ice extent in the Cordillera and in the High Arctic at that time was probably similar to pre...
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Veröffentlicht in: | Quaternary science reviews 2002, Vol.21 (1), p.9-31 |
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