The Late Weichselian glacial maximum in western Svalbard
✍ Scribed by JAN MANGERUD; MAGNE BOLSTAD; ANNE ELGERSMA; DAG HELLIKSEN; JON Y. LANDVIK; ANNE KATRINE LYCKE; IDA LØNNE; OTTO SALVIGSEN; TOM SANDAHL; HANS PETTER SEJRUP
- Book ID
- 111416245
- Publisher
- Co-Action Publishing
- Year
- 1987
- Tongue
- English
- Weight
- 357 KB
- Volume
- 5
- Category
- Article
- ISSN
- 0800-0395
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Younger Dryas cirque glaciers are known to have existed beyond the Scandinavian Ice Sheet in parts of western Norway. At Kråkenes, on the outermost coast, a cirque glacier formed and subsequently wasted away during the Younger Dryas. No glacier existed there during the Allerød. Large cirque moraines
A fully integrated ice-sheet and glacio-isostatic numerical model was run in order to investigate the crustal response to ice loading during the Late Weichselian glaciation of the Barents Sea. The model was used to examine the hypothesis that relative reductions in water depth, caused by glacio-isos