Vis enkel innførsel

dc.contributor.authorHolmsen, Per
dc.coverage.spatial15192 Folldal
dc.date.accessioned2020-08-26T13:05:59Z
dc.date.available2020-08-26T13:05:59Z
dc.date.issued1968
dc.identifier.urihttps://hdl.handle.net/11250/2674894
dc.description.abstractThe present paper is a criticism and a contradiction of J. Gjessing's theory (Gjessing, 1960, 1966) of a subglacial formation of deposits that are actually terraces and bottom sediments of a former glacial (ice-dammed) lakes in East-Central Norway. Gjessing's primary objection against the existence of these lakes led to akward misinterpretations, the most unreasonable consequences and exaggerations of which are stressed critically, in particular his views concerning the following four principal themes: 1. The flat-lying beds in terraces. 2. The shore-lines of former glacial lakes. 3. The \"sheet-like drainage\". 4. The \"ground water level\" within, and below the dead ice body.
dc.language.isonor
dc.relation.ispartofseriesNGU (255)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectAVSETNING
dc.subjectBRESJØAVSETNING
dc.subjectGLASIALGEOLOGI
dc.titleBredemte sjøer eller subglaciale avsetninger?
dc.typeJournal article
dc.description.localcode34953
dc.source.pagenumber97-104


Tilhørende fil(er)

Thumbnail

Denne innførselen finnes i følgende samling(er)

  • Artikler [1063]
    Artikler fra seriene NGU, NGU Bulletin og NGU Skrifter

Vis enkel innførsel

Navngivelse 4.0 Internasjonal
Med mindre annet er angitt, så er denne innførselen lisensiert som Navngivelse 4.0 Internasjonal