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A preliminary study of Lofoten as a potential World Heritage Site based on natural criteria

dc.contributor.authorOlesen, Odleiv
dc.contributor.authorLongva, Oddvar
dc.contributor.authorBargel, Terje
dc.contributor.authorNordgulen, Øystein
dc.contributor.authorOttesen, Dag
dc.coverage.spatialRØST
dc.coverage.spatialVESTVÅGØY
dc.coverage.spatialFLAKSTAD
dc.coverage.spatialMOSKENES
dc.coverage.spatialVÅGAN
dc.coverage.spatialVÆRØY
dc.date.accessioned2020-07-15T07:50:43Z
dc.date.available2020-07-15T07:50:43Z
dc.date.issued2005
dc.identifier.issn0800-3416
dc.identifier.urihttps://hdl.handle.net/11250/2664958
dc.description.abstract(Forkortet)\rThe geology of the Lofoten region has been described with the aim of assessing whether or not the area would qualify as a candidate for the World Heritage List based on its natural properties.\rThe Lofoten archipelago consists mainly of Palaeoproterozoic rocks, including paragneisses and younger plutons (ca 1800 Ma) of the anorthosite-mangerite-charnokite-granite (AMCG) suite. The Precambiran basement of the Lofoten and the adjoining Vesterålen islands is part of a NNE-trending basement high that is overlain to the east by a stack of allochthonous nappes occupying the central axis of the Scandinavian Caledonides.
dc.language.isoeng
dc.relation.ispartofseriesNGU-Rapport (2005.086)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectFJORD
dc.subjectBRE
dc.subjectGEOFYSIKK
dc.subjectGEOMORFOLOGI
dc.titleA preliminary study of Lofoten as a potential World Heritage Site based on natural criteria
dc.typeReport
dc.description.localcode52637
dc.source.pagenumber27 s.
dc.relation.project(312200) Lofoten; geofaglig vurdering av verdensarvområde


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Navngivelse 4.0 Internasjonal
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