Glacial history of interior Jameson Land, East Greenland
The plateaus between 400 and 800 m a.s.l. around the water-divides on central and eastern Janieson Land are covered by the ‘Jameson Land Drift’ up to 50 m thick glacial. placiotluvial and glaciolacustrine deposits. A high content of far-travelled wcsterii rocks indicates the overriding by extensive...
| Published in: | Boreas |
|---|---|
| Main Authors: | , , , |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
John Wiley & Sons Inc.
1994
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| Subjects: | |
| Online Access: | https://lup.lub.lu.se/record/092e0260-5b72-4076-9ace-4a9654acbd59 https://doi.org/10.1111/j.1502-3885.1994.tb00604.x |