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dc.contributor.authorReusch, Hans
dc.coverage.spatial16174 Gjende
dc.coverage.spatial16171 Sikkilsdalen
dc.coverage.spatial16183 Glittertinden
dc.coverage.spatial16182 Sjodalen
dc.coverage.spatialVINJE
dc.coverage.spatialTINN
dc.coverage.spatialNORE OG UVDAL
dc.coverage.spatialHOL
dc.coverage.spatialTELEMARK
dc.coverage.spatialVIKEN
dc.coverage.spatialINNLANDET
dc.coverage.spatialVESTLAND
dc.date.accessioned2020-08-26T12:36:58Z
dc.date.available2020-08-26T12:36:58Z
dc.date.issued1894
dc.identifier.urihttps://hdl.handle.net/11250/2674524
dc.description.abstractLangfjeldene is the great mountainridge, which runs through southern Norway. Mr.Andr.M.Hansen have forwarded the hypothesis, that in the region east of it (map p. 52) there existed at the end of the ice-age large lakes dammed in by the last rests of the melting ice. The present author does not find that there are reasons for such a supposition. Some inland \"strand-lines\" from the northermost part of the region under consideration age figured on page 59. If they marke shores of ancient lakes (which is not at all sure), it is quite a local phenomenon.
dc.language.isonor
dc.relation.ispartofseriesNGU (14)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectMORENE
dc.subjectAVSETNING
dc.subjectSTRANDFORSKYVNING
dc.subjectBREBEVEGELSE
dc.titleHar der existeret store, isdæmmede indsjøer paa østsiden av Langfjeldene?
dc.typeJournal article
dc.description.localcode36139
dc.source.pagenumber51-59


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