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dc.contributor.authorRekstad, Johan
dc.coverage.spatial17271 Træna Fyr
dc.coverage.spatial17282 Træna
dc.coverage.spatial12154 Bruvik
dc.coverage.spatial12153 Fusa
dc.coverage.spatial12152 Varaldsøy
dc.coverage.spatial12151 Strandebarm
dc.coverage.spatial13154 Jondal
dc.coverage.spatial13151 Ullensvang
dc.coverage.spatialVESTLAND
dc.coverage.spatialNORDLAND
dc.coverage.spatialULVIK
dc.coverage.spatialULLENSVANG
dc.coverage.spatialVOSS
dc.coverage.spatialKVAM
dc.coverage.spatialBJØRNAFJORDEN
dc.coverage.spatialKVINNHERAD
dc.coverage.spatialSAMNANGER
dc.coverage.spatialEIDFJORD
dc.coverage.spatialTRÆNA
dc.coverage.spatial14163 Myrdal
dc.coverage.spatial13162 Ulvik
dc.date.accessioned2020-08-26T13:28:54Z
dc.date.available2020-08-26T13:28:54Z
dc.date.issued1911
dc.identifier.urihttps://hdl.handle.net/11250/2675197
dc.description.abstractForkortet:The region described is situated in Western Norway on the NW-side of theHardangerfjord between 60\u00B0 6' and 60\u00B0 40' N. At the close of the Ice Age theland lay lower than at present. Raised beaches and terraces mark thatsubmersion. From that time to the present the land has risen, in the westernpart of the district about 70 m and in the eastern part about 124 m. Fromthe mollusk-shells found in the terraces it is to be seen that the climatewas cold during the maximum of subsidence, but it grew milder as the land rise.The rise was interrupted by a submersion of short duration, theTapes-submersion, during which the climate was milder than at present.
dc.language.isonor
dc.relation.ispartofseriesNGU (59)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectKVARTÆRGEOLOGI
dc.subjectKARTLEGGING
dc.subjectMALMGEOLOGI
dc.subjectOMDANNET BERGART
dc.subjectPETROGRAFI
dc.subjectSTØRKNINGSBERGART
dc.titleII. Geologiske iagttagelser fra nordvestsiden av Hardangerfjord
dc.typeJournal article
dc.description.localcode35918
dc.source.pagenumber62


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