dc.contributor.author | Reite, Arne J. | |
dc.coverage.spatial | 16214 Trondheim | |
dc.coverage.spatial | MALVIK | |
dc.coverage.spatial | TRONDHEIM | |
dc.date.accessioned | 2020-08-26T13:25:54Z | |
dc.date.available | 2020-08-26T13:25:54Z | |
dc.date.issued | 1983 | |
dc.identifier.uri | https://hdl.handle.net/11250/2675173 | |
dc.description.abstract | The 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.iso | nor | |
dc.relation.ispartofseries | NGU; Skrifter (391; 46) | |
dc.rights | Navngivelse 4.0 Internasjonal | |
dc.rights.uri | http://creativecommons.org/licenses/by/4.0/deed.no | |
dc.subject | KARTLEGGING | |
dc.subject | AVSETNING | |
dc.subject | GLASIALGEOLOGI | |
dc.subject | STRANDFORSKYVNING | |
dc.subject | SEISMISK PROFIL | |
dc.subject | GEOKRONOLOGI | |
dc.title | Trondheim. Beskrivelse til kvartærgeologisk kart 1621 IV - M 1:50 000 (med fargetrykt kart). | |
dc.type | Journal article | |
dc.description.localcode | 35146 | |
dc.source.pagenumber | 44+kart | |