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dc.contributor.authorReite, Arne J.
dc.coverage.spatial16214 Trondheim
dc.coverage.spatialMALVIK
dc.coverage.spatialTRONDHEIM
dc.date.accessioned2020-08-26T13:25:54Z
dc.date.available2020-08-26T13:25:54Z
dc.date.issued1983
dc.identifier.urihttps://hdl.handle.net/11250/2675173
dc.description.abstractThe superficial deposits within the map-sheet Trondheim, Central Norway, are classified and described. The mountains generally have a thin and discontinuous cover of till. In the lowland areas fine-grained marine sediments dominate; these were deposited at a sea level c. 180 m higher than the present one. The ice-sheet receded before 11,000 B.P., followed by an advance to the Ekle-Tiller Moraines during the first half of the Younger Dryas Chronozone. The Brøttem Moraines, situated in the southeastern part of the map-area, were deposited during a younger glacial advance. Short accounts are given on shoreline displacement, river erosion and slides. The potential for different utilization of the superficial deposits is also briefly discussed.
dc.language.isonor
dc.relation.ispartofseriesNGU; Skrifter (391; 46)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectKARTLEGGING
dc.subjectAVSETNING
dc.subjectGLASIALGEOLOGI
dc.subjectSTRANDFORSKYVNING
dc.subjectSEISMISK PROFIL
dc.subjectGEOKRONOLOGI
dc.titleTrondheim. Beskrivelse til kvartærgeologisk kart 1621 IV - M 1:50 000 (med fargetrykt kart).
dc.typeJournal article
dc.description.localcode35146
dc.source.pagenumber44+kart


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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