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dc.contributor.authorOlsen, Lars
dc.contributor.authorSveian, Harald
dc.contributor.authorHøgaas, Fredrik
dc.coverage.spatialLEVANGER
dc.coverage.spatialFROSTA
dc.coverage.spatial16222 Frosta
dc.coverage.spatial16223 Leksvik
dc.date.accessioned2020-08-26T09:05:50Z
dc.date.available2020-08-26T09:05:50Z
dc.date.issued2015
dc.identifier.issn1894-7913
dc.identifier.urihttps://hdl.handle.net/11250/2674162
dc.description.abstractThe ice-marginal Tautra and Hoklingen Substages in the Trøndelag counties, Mid-Norway, have for a long time been referred to as of early and late Younger Dryas (YD) age, respectively. The basis for this is the regional distribution and morphological correlations of the associated moraines and a number of 14C- datings, mainly of marine shells, previously presented in different papers and map-sheets. In this overview article we present a collection of all 14C-dates associated (more or less accurately) with the Tautra and Hoklingen Substages, a number of 49 and 27 respectively.
dc.language.isoeng
dc.relation.ispartofseriesNGU Bulletin (454)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectISAVSMELTING
dc.subjectKVARTÆRGEOLOGI
dc.subjectDATERING
dc.subjectGEOMORFOLOGI
dc.titleAge of the Younger Dryas ice-marginal substages in Mid-Norway - Tautra and Hoklingen, based on a compilation of 14C-dates
dc.typeJournal article
dc.description.localcode63776
dc.source.pagenumber1-13


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