Bredemte sjøer eller subglaciale avsetninger?

dc.contributor.author	Holmsen, Per
dc.coverage.spatial	15192 Folldal
dc.date.accessioned	2020-08-26T13:05:59Z
dc.date.available	2020-08-26T13:05:59Z
dc.date.issued	1968
dc.identifier.uri	https://hdl.handle.net/11250/2674894
dc.description.abstract	The 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.iso	nor
dc.relation.ispartofseries	NGU (255)
dc.rights	Navngivelse 4.0 Internasjonal
dc.rights.uri	http://creativecommons.org/licenses/by/4.0/deed.no
dc.subject	AVSETNING
dc.subject	BRESJØAVSETNING
dc.subject	GLASIALGEOLOGI
dc.title	Bredemte sjøer eller subglaciale avsetninger?
dc.type	Journal article
dc.description.localcode	34953
dc.source.pagenumber	97-104

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