Rekonstruksjon av isavsmeltingsforløpet i Gråsteindal-området, indre Sunnmøre
The North-Western part of Norway became ice free during the Late Weichselian glaciation and the ice margin is mapped across several fjord districts. Distinct moraine systems in the high mountains indicate an extensive local glaciation during the Younger Dryas. The purpose of this thesis is to recons...
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| Format: | Master Thesis |
| Language: | Bokmål |
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The University of Bergen
2017
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| Online Access: | https://hdl.handle.net/1956/17237 |