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dc.contributor.authorHorn, Gunnar
dc.coverage.spatial20274 Storforshei
dc.coverage.spatial19271 Mo i Rana
dc.coverage.spatial19282 Svartisen
dc.coverage.spatial19281 Glomfjord
dc.coverage.spatialMELØY
dc.coverage.spatialRANA
dc.date.accessioned2020-08-26T12:39:21Z
dc.date.available2020-08-26T12:39:21Z
dc.date.issued1947
dc.identifier.urihttps://hdl.handle.net/11250/2674554
dc.description.abstractThe cave passages are mostly tunnel shaped, usually with a circular or elliptical section. These passages were formed when they were completely water-filled. Underground streams have later made cuts into the floor of some of the passages. The view presented as to the origin of the caves may be termed the subglacial theory of cave excavation.
dc.language.isonor
dc.relation.ispartofseriesNGU (165)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectKALKSTEIN
dc.subjectGEOMORFOLOGI
dc.subjectKARTLEGGING
dc.subjectBERGGRUNNSGEOLOGI
dc.subjectPLANTEGRUPPE
dc.subjectFOSSIL
dc.titleKarsthuler i Nordland.
dc.typeJournal article
dc.description.localcode34970
dc.source.pagenumber1-77


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    Artikler fra seriene NGU, NGU Bulletin og NGU Skrifter

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