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dc.contributor.authorHolmsen, Gunnar
dc.coverage.spatial16192 Tylldal
dc.coverage.spatial16191 Tynset
dc.coverage.spatial19184 Hanestad
dc.coverage.spatial19181 Rendalen
dc.coverage.spatialTOLGA
dc.coverage.spatialTYNSET
dc.coverage.spatialALVDAL
dc.coverage.spatialRENDALEN
dc.date.accessioned2020-08-26T13:31:00Z
dc.date.available2020-08-26T13:31:00Z
dc.date.issued1916
dc.identifier.urihttps://hdl.handle.net/11250/2675225
dc.description.abstractThe present paper forms a supplement to the author's: Ice-dammed lakes of Northern Østerdal, NGU nr. 73. The lowest sete-building lake in the Glommen valley has extended its branches into the valleys Rendalen, Tydalen and Brydalen, and has formed seter and shore-lines of just the same kind as the main valley. Last summer the author examined these shorelines more closely and determined their exact heights above the sea. The measurements are founded on the trigonometrical points of the district, the hights of which are again in connection with the cairn at Tronfjell, this point being accurately levelled by the Norwegian Geographical Survey.
dc.language.isonor
dc.relation.ispartofseriesNGU (79)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectKARTLEGGING
dc.subjectAVSETNING
dc.subjectBRESJØAVSETNING
dc.subjectMORENE
dc.subjectGLASIALGEOLOGI
dc.subjectSTRANDAVSETNING
dc.titleI. Rendalens bræsjø
dc.typeJournal article
dc.description.localcode35450
dc.source.pagenumber38


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