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dc.contributor.authorSkålvoll, Harald
dc.coverage.spatial20344 Skoganvarre
dc.coverage.spatial20341 Hal'kavarri
dc.coverage.spatial20353 Lakselv
dc.coverage.spatial20352 Mun'kavarri
dc.date.accessioned2020-08-26T12:50:47Z
dc.date.available2020-08-26T12:50:47Z
dc.date.issued1960
dc.identifier.urihttps://hdl.handle.net/11250/2674716
dc.description.abstractSome observations of quaternary deposits in Lakselvdalen, Finnmark: Glacial striae and erratics show that the ice has moved from south to north. Ground moraine, dead ice moraine, marine and glacial-fluvial deposits occur. Terraces are formed in the marine deposits at 5 to 70 m above sea level. In the glacial fluvial deposits two terraces are found, 75 and 85 meter above sea level. The occurrence of dead ice moraine and several kettel holes in the highest terraces show that the ice was \"dead\" when it melted away from this area.
dc.language.isonor
dc.relation.ispartofseriesNGU (211)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectMARIN AVSETNING
dc.subjectKARTLEGGING
dc.subjectAVSETNING
dc.subjectGLASIALGEOLOGI
dc.subjectMORENE
dc.subjectBREELVAVSETNING
dc.titleNoen kvartærgeologiske iakttagelser i Lakselvdalen, Finnmark.
dc.typeJournal article
dc.description.localcode35602
dc.source.pagenumber119-123


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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