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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Bibliographic Details
Main Author: Follestad, Bjørn A.
Format: Article in Journal/Newspaper
Language:English
Published: 2003
Subjects:
Online Access:https://hdl.handle.net/11250/2674104