Glacial history of western Norway 15,000–10,000 B.P.
The deglaciation patterns of the Bergen and Nordfjord‐Sunnmøre areas in western Norway are described and correlated. In the Bergen area the coast was first deglaciated at 12,600 B.P., with a succeeding re‐advance into the North Sea around 12,200 B.P. Later, during the Allerød, the inland ice retreat...
| Published in: | Boreas |
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| Main Authors: | , , , |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
Wiley
1979
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| Subjects: | |
| Online Access: | http://dx.doi.org/10.1111/j.1502-3885.1979.tb00798.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1502-3885.1979.tb00798.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1502-3885.1979.tb00798.x |
| Summary: | The deglaciation patterns of the Bergen and Nordfjord‐Sunnmøre areas in western Norway are described and correlated. In the Bergen area the coast was first deglaciated at 12,600 B.P., with a succeeding re‐advance into the North Sea around 12,200 B.P. Later, during the Allerød, the inland ice retreated at least 50 km, but nearly reached the sea again during the Younger Dryas re‐advance, ending at 10,000 B.P. Sunnmøre was ice‐free during an interstadial 28,000–38,000 B.P. Later the inland ice reached the sea. The final deglaciation is poorly dated in Sunnmøre, while further south in Nordfjord, it started slightly before 12,300 B.P., followed by a major retreat. No large re‐advance of the inland ice occurred during the Younger Dryas. However, in the Sunnmøre‐Nordfjord area many local glaciers formed outside the inland ice during the Younger Dryas. Limnic sediments outside one such cirque glacier have been cored and dated, proving that the glacier did not exist at 12,300‐11,000 B.P., and that it was formed and disappeared in the time interval 11,000–10,000 B.P. (Younger Dryas). The erosion rate of the cirque glacier was 0.9 mm/year. |
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