Noen kvartærgeologiske iakttagelser i Lakselvdalen, Finnmark.
Some observations of quaternary deposits in Lakselvdalen, Finnmark: Glacial striae and erratics show that the ice has moved from south to north. Ground moraine, dead ice moraine, marine and glacial-fluvial deposits occur. Terraces are formed in the marine deposits at 5 to 70 m above sea level. In th...
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Format: | Article in Journal/Newspaper |
Language: | Norwegian |
Published: |
1960
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Online Access: | https://hdl.handle.net/11250/2674716 |