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dc.contributor.authorFollestad, Bjørn A.
dc.coverage.spatial18183 Ringebu
dc.coverage.spatial18184 Atnsjøen
dc.coverage.spatial18182 Imsdalen
dc.date.accessioned2020-08-26T09:04:09Z
dc.date.available2020-08-26T09:04:09Z
dc.date.issued2001
dc.identifier.urihttps://hdl.handle.net/11250/2674127
dc.description.abstractOn the basis of different field observations, several authors have discussed the form of the inland ice in southern Norway. In this work, lateral features indicating the upper limit of zones of meltwater drainage marked by meltwater channels are used for the reconstruction of two distinct ice surfaces during the deglaciation of the valley Atndalen. Through the mapping of these features a detailed image of the deglaciation can be obtained and also be used for regional correction of the ice surface.
dc.language.isoeng
dc.relation.ispartofseriesNGU Bulletin (438)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectGLASIAL FORM
dc.subjectGLASIALGEOLOGI
dc.subjectISAVSMELTING
dc.titleThe surface of the inland ice in the Atndalen valley, South-central Norway.
dc.typeJournal article
dc.description.localcode49800
dc.source.pagenumber15-19


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