En rekonstruksjon av isutbredelsen i Rondane gjennom Weichsel med hovedvekt på glasialgeologi og isavsmeltingsformer
The Rondane area has since the 18th century been of interest for scientists because of its glaciofluvial deposits (Gjessing, 1960), large number of periglacial phenomena (Barchs & Treter, 1976; Shakesby et al., 1987), and because the area is suggested to have been covered by the inland ice sheet...
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| Format: | Master Thesis |
| Language: | Bokmål |
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The University of Bergen
2003
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| Online Access: | https://hdl.handle.net/1956/1590 |