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A proposed deglaciation chronology for the Trondheimsfjord area, Central Norway.

dc.contributor.authorReite, Arne J.
dc.contributor.authorSveian, Harald
dc.contributor.authorSelnes, H.
dc.coverage.spatialSTEINKJER
dc.coverage.spatialÅFJORD
dc.coverage.spatialINDRE FOSEN
dc.coverage.spatialTRONDHEIM
dc.coverage.spatialINDERØY
dc.coverage.spatialLEVANGER
dc.date.accessioned2020-08-26T13:21:40Z
dc.date.available2020-08-26T13:21:40Z
dc.date.issued1982
dc.identifier.urihttps://hdl.handle.net/11250/2675131
dc.description.abstractRadiocarbon datings of the deglaciation of the Trondheimsfjord area strongly suggest that the coastal areas and the outer part of the fjord were deglaciated before 11000 B.P. During early Younger Dryas the inland ice advanced to the Tautra Moraines (10800-10500 B.P.). Further inland the Hoklingen Moraines (10300-10100 B.P.) and the Vuku Moraines (c. 9800 P.B.) were deposited during marked glacial advances. Other ice-marginal deposits are mostly dependent on local topography. Brief comments are given on the shoreline displacement during the deglaciation.
dc.language.isoeng
dc.relation.ispartofseriesNGU (373)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectDATERING
dc.subjectISAVSMELTING
dc.subjectMORENE
dc.titleA proposed deglaciation chronology for the Trondheimsfjord area, Central Norway.
dc.typeJournal article
dc.description.localcode35659
dc.source.pagenumber75 - 84


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