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dc.contributor.authorReusch, Hans
dc.coverage.spatial16161 Tisleia
dc.coverage.spatial17164 Aurdal
dc.coverage.spatial17161 Bruflat
dc.coverage.spatial16174 Gjende
dc.coverage.spatial16173 Vangsmjøsi
dc.coverage.spatial16172 Slidre
dc.coverage.spatial16171 Sikkilsdalen
dc.coverage.spatialØYSTRE SLIDRE
dc.coverage.spatialETNEDAL
dc.coverage.spatialVESTRE SLIDRE
dc.coverage.spatialNORD-AURDAL
dc.coverage.spatialVANG OPPLAND
dc.coverage.spatialSØR-AURDAL
dc.date.accessioned2020-08-26T12:36:46Z
dc.date.available2020-08-26T12:36:46Z
dc.date.issued1894
dc.identifier.urihttps://hdl.handle.net/11250/2674519
dc.description.abstractForkortet: Bygdin is a mountain-lake in central Norway at 61\u00B0 20' N. Bagn is a place farther to the South at 60\u00B0 50' N. On the schematic birds-eye-view p. 18 Bygdin lies at J; Bagn at Bg. The base of the Archaean, in which the deeper parts of the valleys are eroded out as seen in the figure. Upon is rests the Cambro-Silurian composed of dark blue-grey quartzitic sandstones and argillaceous schists; the fosils are few. Overlying this there is a light reddish and greyish sandstone (the dotted mountain Mellane at M. in the figure). The distant mountains at J. consist of gabbro and allied rocks of eruptive origin. A section of Mellane (M.) is found on p. 28. Cambrian fossils (etasje 1) are discovered by the present author in the schists at G. and Ordovician fossils (etasje 3) by Mr.Bjørlykke at J. The uppermost part of the mountain consist of lightcoloured sandstone, which in its appearance is not much different from many vareties of true Cambrian \"sparagmite\". We must consequently in the future discriminate between two \"sparagmites\" in central Norway.
dc.language.isonor
dc.relation.ispartofseriesNGU (14)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectSTØRKNINGSBERGART
dc.subjectPETROGRAFI
dc.subjectSEDIMENTÆR BERGART
dc.subjectKVARTÆRGEOLOGI
dc.subjectOMDANNET BERGART
dc.subjectKART
dc.titleMellem Bygdin og Bang
dc.typeJournal article
dc.description.localcode36138
dc.source.pagenumber15-50


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