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Glasialgeologi og vegetasjonsinnvandring i Indre Nordhordland, Vest-Norge.

dc.contributor.authorAa, Asbjørn Rune
dc.contributor.authorMangerud, Jan
dc.coverage.spatial12163 Stanghelle
dc.coverage.spatial12162 Evanger
dc.coverage.spatial12161 Eksingedal
dc.coverage.spatial13164 Myrkdalen
dc.coverage.spatial13163 Voss
dc.coverage.spatialMODALEN
dc.coverage.spatialVAKSDAL
dc.coverage.spatialVOSS
dc.coverage.spatial12164 Mo
dc.date.accessioned2020-08-26T13:20:35Z
dc.date.available2020-08-26T13:20:35Z
dc.date.issued1981
dc.identifier.urihttps://hdl.handle.net/11250/2675109
dc.description.abstractIn the area between Hardangerfjorden and Sognefjorden an oldest regional ice movement towards the west has been reconstructed. Younger regional ice movements were towards south-west in the southern parts. Therefore, an east-west ice divide was present in the Stølsheimen area. The immigration of Corylus and Alnus appears to be 800-1000 years delayed, compared with the western coast of Hordaland. The pollen diagrams indicate a Holocene vegetational history with more similarities with inland sites than with coastal sites.
dc.language.isoeng
dc.relation.ispartofseriesNGU (369)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectGLASIALGEOLOGI
dc.subjectPOLLEN
dc.subjectSTRANDFORSKYVNING
dc.subjectISAVSMELTING
dc.titleGlasialgeologi og vegetasjonsinnvandring i Indre Nordhordland, Vest-Norge.
dc.typeJournal article
dc.description.localcode36256
dc.source.pagenumber33 - 75


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