dc.contributor.author | Follestad, Bjørn A. | |
dc.coverage.spatial | 15203 Oppdal | |
dc.date.accessioned | 2020-08-26T09:03:00Z | |
dc.date.available | 2020-08-26T09:03:00Z | |
dc.date.issued | 2003 | |
dc.identifier.uri | https://hdl.handle.net/11250/2674104 | |
dc.description.abstract | 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 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.iso | eng | |
dc.relation.ispartofseries | NGU Bulletin (441) | |
dc.rights | Navngivelse 4.0 Internasjonal | |
dc.rights.uri | http://creativecommons.org/licenses/by/4.0/deed.no | |
dc.subject | GLASIAL FORM | |
dc.subject | GLASIALGEOLOGI | |
dc.subject | ISAVSMELTING | |
dc.title | Development of minor late-glacial ice domes east of Oppdal, Central Norway | |
dc.type | Journal article | |
dc.description.localcode | 50693 | |
dc.source.pagenumber | 39-49 | |