Show simple item record

dc.contributor.authorLasca, N.P.
dc.coverage.spatial14211 Hemne
dc.date.accessioned2020-08-26T13:08:49Z
dc.date.available2020-08-26T13:08:49Z
dc.date.issued1970
dc.identifier.urihttps://hdl.handle.net/11250/2674928
dc.description.abstractFour radiocarbon dates are used to date moraines in the inner Hemnefjord area. The radiometric ages of moraines range from approximately 10,720 to 11,310 years B.P. and probably correlate with the Ra moraines in Southern Norway and the Tromsø-Lyngen and Skardmunken moraines in Northern Norway. Evidence suggests that by 11,300 years B.P. the Hemnefjord was partially open to the sea. The Hemne substage's ice either extended to the coast on both sides of an open fjord system, or local glciers persisted in the outer fjord when the Hemne substage's ice was in the inner Hemnefjord.
dc.language.isoeng
dc.relation.ispartofseriesNGU (266)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectGEOKRONOLOGI
dc.subjectGLASIALGEOLOGI
dc.subjectAVSETNING
dc.subjectFOSSIL
dc.subjectGLASIAL FORM
dc.titleMoraines in the Hemnefjord area, Western Norway.
dc.typeJournal article
dc.description.localcode34877
dc.source.pagenumber62-69


Files in this item

Thumbnail

This item appears in the following Collection(s)

  • Artikler [1063]
    Artikler fra seriene NGU, NGU Bulletin og NGU Skrifter

Show simple item record

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