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dc.contributor.authorTollan, Arne
dc.coverage.spatial16184 Lom
dc.coverage.spatial16181 Vågå
dc.coverage.spatial14193 Lesjaskog
dc.coverage.spatial14192 Dombås
dc.coverage.spatialLOM
dc.coverage.spatialVÅGÅ
dc.coverage.spatialLESJA
dc.date.accessioned2020-08-26T12:54:50Z
dc.date.available2020-08-26T12:54:50Z
dc.date.issued1963
dc.identifier.urihttps://hdl.handle.net/11250/2674779
dc.description.abstractGlacial striae and ice-moulded forms indicate that the earliest direction of glacial flow was towards E, and that the flow at the maximum was towards N or NW. The late-glacial movement, however, seems to have been towards NE, in particular because the long axes in recently discovered drumlins have this orientation. The corresponding centre of active glaciation was situated in the northern part of the Jotunheimen high mountain area, at a time when the remaining ice, east of the investigated area, was climatically dead. The deglaciation period brought large amounts of melt water to the area. Magnificent clean-swept belts show the former water ways. During this stage considerable quantities of sand and gravel were carried to the valley bottoms successively. The transport history was partly complicated. A general tendency to subglacial transport and accumulation seems to have occurred in particular during the first phase, at a given place. Later, sublateral and\/or lateral transport, modifying the earlier accumulation forms, have taken place. On the mountain slopes sublateral drainage channels are common, in part cutting across earlier subglacial accumulations.
dc.language.isonor
dc.relation.ispartofseriesNGU (223)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectPETROGRAFI
dc.subjectISAVSMELTING
dc.subjectBREBEVEGELSE
dc.subjectAVSETNING
dc.subjectSTØRKNINGSBERGART
dc.subjectGLASIALGEOLOGI
dc.titleTrekk av isbevegelsen og isavsmeltningen i Nordre Gudbrandsdalens fjelltrakter.
dc.typeJournal article
dc.description.localcode35353
dc.source.pagenumber328-345


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    Artikler fra seriene NGU, NGU Bulletin og NGU Skrifter

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