Glaciala och fluviala dalgångar i södra Norge : Ett resultat av mesozoisk sprickbildning och kenozoisk erosion
The dramatic landscape of Norway has a long history of different events during the Phanerozoic. During the Caledonian orogeny, the basement became fractured, and during the warm climate in the Mesozoic, the fractures became deeply weathered. These fracture systems later became eroded, forming the ma...
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| Format: | Others |
| Language: | Swedish |
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Uppsala universitet, Kulturgeografiska institutionen
2019
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| Online Access: | http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-427256 |