Glasialgeologi og vegetasjonsinnvandring i Indre Nordhordland, Vest-Norge.

dc.contributor.author	Aa, Asbjørn Rune
dc.contributor.author	Mangerud, Jan
dc.coverage.spatial	12163 Stanghelle
dc.coverage.spatial	12162 Evanger
dc.coverage.spatial	12161 Eksingedal
dc.coverage.spatial	13164 Myrkdalen
dc.coverage.spatial	13163 Voss
dc.coverage.spatial	MODALEN
dc.coverage.spatial	VAKSDAL
dc.coverage.spatial	VOSS
dc.coverage.spatial	12164 Mo
dc.date.accessioned	2020-08-26T13:20:35Z
dc.date.available	2020-08-26T13:20:35Z
dc.date.issued	1981
dc.identifier.uri	https://hdl.handle.net/11250/2675109
dc.description.abstract	In 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.iso	eng
dc.relation.ispartofseries	NGU (369)
dc.rights	Navngivelse 4.0 Internasjonal
dc.rights.uri	http://creativecommons.org/licenses/by/4.0/deed.no
dc.subject	GLASIALGEOLOGI
dc.subject	POLLEN
dc.subject	STRANDFORSKYVNING
dc.subject	ISAVSMELTING
dc.title	Glasialgeologi og vegetasjonsinnvandring i Indre Nordhordland, Vest-Norge.
dc.type	Journal article
dc.description.localcode	36256
dc.source.pagenumber	33 - 75

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