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dc.contributor.authorFollestad, Bjørn A.
dc.coverage.spatial15203 Oppdal
dc.date.accessioned2020-08-26T09:03:00Z
dc.date.available2020-08-26T09:03:00Z
dc.date.issued2003
dc.identifier.urihttps://hdl.handle.net/11250/2674104
dc.description.abstractGlacial 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 the major northwesterly-directed flow and is correlated with the early YD marginal deposits in the Storås area. A marked, younger, westerly-directed iceflow from a late-glacial dome east of the Oppdal area is thought to correspon with the Hoklingen ice-marginal deposits dated to the late YD Chronozone in the Trondheimsfjord district. In the main Oppdal-Fagerhaug-Berkåk valley, this younger ice flow turned to the southwest and can be traced southwards to the Oppdal area where it joined the remnants of a glacier in the Drivdalen valley.
dc.language.isoeng
dc.relation.ispartofseriesNGU Bulletin (441)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectGLASIAL FORM
dc.subjectGLASIALGEOLOGI
dc.subjectISAVSMELTING
dc.titleDevelopment of minor late-glacial ice domes east of Oppdal, Central Norway
dc.typeJournal article
dc.description.localcode50693
dc.source.pagenumber39-49


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Navngivelse 4.0 Internasjonal
Except where otherwise noted, this item's license is described as Navngivelse 4.0 Internasjonal