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dc.contributor.authorReusch, Hans
dc.coverage.spatial12154 Bruvik
dc.coverage.spatial12163 Stanghelle
dc.coverage.spatial12152 Varaldsøy
dc.coverage.spatial12161 Eksingedal
dc.coverage.spatial13164 Myrkdalen
dc.coverage.spatial13163 Voss
dc.coverage.spatial13162 Ulvik
dc.coverage.spatial13161 Gudvangen
dc.coverage.spatialVOSS
dc.coverage.spatialKVAM
dc.coverage.spatialVAKSDAL
dc.date.accessioned2020-08-26T13:26:41Z
dc.date.available2020-08-26T13:26:41Z
dc.date.issued1905
dc.identifier.urihttps://hdl.handle.net/11250/2675183
dc.description.abstractForkortet:The Western gneiss region. The lightest red in the map is gneiss, the darkestred is an amphibole-bearing rock, the Evanger diorite, mostly made schistoseby compression; the middle red represents granite the structure of which is asa rule foliated particularly by the parallel position of the laminae of mica.Many excellent cuttings may be studied along the railway westwards from theVangs Lake. The figures on p.12 and the following pages are from this locality.Figures on p.12 and the following pages are from this locality. I and II showlight coarse-grained granite in diorite with planeparallel structure. It isinteresting to note, that the mica within the granite has assumed a positionin accordance with the structure of the environing. In the next figuredifferent varieties of the compressed dioritic rock occur together giving theimpression of stratification.
dc.language.isonor
dc.relation.ispartofseriesNGU (40)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectKARTLEGGING
dc.subjectGEOMORFOLOGI
dc.subjectKVARTÆRGEOLOGI
dc.subjectOMDANNET BERGART
dc.subjectPETROGRAFI
dc.subjectSTØRKNINGSBERGART
dc.titleVoss. Fjeldbygningen inden rektangelkartet Voss's omraade
dc.typeJournal article
dc.description.localcode36020
dc.source.pagenumber76


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