Development of minor late-glacial ice domes east of Oppdal, Central Norway
Glacial striations and ice-marginal forms such as lateral moraines and meltwater channels show that a major north-westerly-directed ice flow invaded the Oppdal area prior to the Younger Dryas (YD) Chronozone. Through the main valley from Oppdal to Fagerhaug and Berkåk, a northerly ice flow followed...
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Format: | Article in Journal/Newspaper |
Language: | English |
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2003
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Online Access: | https://hdl.handle.net/11250/2674104 |