Ice-dammed lake and ice-margin evolution during the Holocene in the Kangerlussuaq area of west Greenland
There is a lack of detailed information on the Holocene evolution of the west Greenland ice margin, not least because it was farther inland than at present and thus at present is covered by ice. Suggestions have been put forward, both of relatively quick ice-margin retreat and of relatively stable i...
Furkejuvvon:
| Váldodahkkit: | , , , |
|---|---|
| Materiálatiipa: | Artigo |
| Giella: | Inglês |
| Almmustuhtton: |
Taylor & Francis Group
2018-01-01
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| Ráidu: | Arctic, Antarctic, and Alpine Research |
| Fáttát: | |
| Liŋkkat: | http://dx.doi.org/10.1080/15230430.2017.1420854 |
| Fáddágilkorat: |
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