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dc.contributor.authorReusch, Hans
dc.date.accessioned2020-08-26T13:15:28Z
dc.date.available2020-08-26T13:15:28Z
dc.date.issued1901
dc.identifier.urihttps://hdl.handle.net/11250/2675030
dc.description.abstractForkortet: Up to the present, the relief of Norway has not been understood sufficiently to allow of a satisfactory explanation being given of even the most salient features, such as the contrast between plateau and valley, which was the subject of a very notable paper by P.A.Munch as much as half a century ago. The Sognefjord, with its adjacent valleys, forms a magnificent system, of which the inner ramifications are surrounded by the loftiest part of our country \"The Great Mountains of Norway\". They enclose in a 3\/4 circle a basin of palaeic high plateaus. The figure on p. 137 is from its outer part, where the relation between plateau and valleys is clearly seen. A great Sogne river and its side streams have eroded the fiord and its many arms in the palaeic surface during a long and eventful history (Map p.140 and p.247). It is stated above that the fiord-valleys were probably formed as well by running water as by ice alternating during interglacial and glacial periods. It is just from the Sogne- fjord that we have proofs that the great glaciers that filled the fiord in the latest glacial period, even if they achieved a fair amount of work, did not obliterate everywhere the vestiges of the previous water erosion.
dc.language.isonor
dc.relation.ispartofseriesNGU (32)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectGEOMORFOLOGI
dc.subjectGEOMORFOLOGI
dc.subjectSTRANDFLATE
dc.subjectGLASIAL FORM
dc.titleNogle bidrag til forstaaelsen af, hvorledes Norges dale og fjelde er blevne til
dc.typeJournal article
dc.description.localcode36096
dc.source.pagenumber124-217


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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