Late Quaternary development of the southern sector of the Greenland Ice Sheet, with particular reference to the Qassimiut lobe
The evolution of the southern Greenland Ice Sheet is interpreted from a synthesis of geological data and palaeoclimatic information provided by the ice‐sheet cores. At the Last Glacial Maximum the ice margin would have been at the shelf break and the ice sheet was fringed by shelf ice. Virtually all...
| Published in: | Boreas |
|---|---|
| Main Authors: | , , |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
Wiley
2004
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| Subjects: | |
| Online Access: | http://dx.doi.org/10.1111/j.1502-3885.2004.tb01242.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1502-3885.2004.tb01242.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1502-3885.2004.tb01242.x |