Glaciation in northern East Greenland during the Late Weichselian and Early Flandrian
The frontal positions of glaciers in fiords, sounds and larger valleys during the glaciation maximum around 10,000 B.P. and the extent of ice‐free areas at that time are shown, together with an isobase map of the altitude of the contemporaneous (or younger) marine limit. A number of 14 C and some Am...
| Published in: | Boreas |
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| Main Author: | |
| Format: | Article in Journal/Newspaper |
| Language: | English |
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Wiley
1979
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| Online Access: | http://dx.doi.org/10.1111/j.1502-3885.1979.tb00812.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1502-3885.1979.tb00812.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1502-3885.1979.tb00812.x |
| Summary: | The frontal positions of glaciers in fiords, sounds and larger valleys during the glaciation maximum around 10,000 B.P. and the extent of ice‐free areas at that time are shown, together with an isobase map of the altitude of the contemporaneous (or younger) marine limit. A number of 14 C and some Amino Acid datings related to the glacial advance, culmination and retreat are presented. Some time after a Middle Weichselian period with restricted glaciation the glaciers advanced and stood at their maximum positions at about 10,300 B.P., in some areas remaining there until about 9500 B.P., at which time sizeable lowland areas outside the ice‐fronts were unglaciated and a large number of nunataks of various types occurred. The retreat of the glaciers started about 10,300 B.P. in the south, but seems to have been delayed towards the north. However, by 9000 B.P. all outer parts of the fiords were deglaciated and their central parts by 8500 B.P. The marine limit synchronous with this glaciation maximum and the deglaciation sinks from a southern maximum value of about 110 m to about 55 m in the north, reflecting a decreasing amplitude of the glacial advance. |
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