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dc.contributor.authorReusch, Hans
dc.coverage.spatial23353 Varangerbotn
dc.coverage.spatialPORSANGER
dc.coverage.spatialHAMMERFEST
dc.coverage.spatialVARDØ
dc.coverage.spatialVADSØ
dc.coverage.spatialTANA
dc.coverage.spatialBERLEVÅG
dc.coverage.spatialBÅTSFJORD
dc.coverage.spatialNESSEBY
dc.coverage.spatial23354 Tana
dc.coverage.spatial23361 Berlevåg
dc.coverage.spatial23363 Trollfjorden
dc.coverage.spatialLEBESBY
dc.coverage.spatial25354 Vardø
dc.coverage.spatial24353 Vadsø
dc.coverage.spatial24354 Skipskjølen
dc.coverage.spatial24362 Syltefjord
dc.coverage.spatial24363 Båtsfjord
dc.coverage.spatial23352 Nesseby
dc.date.accessioned2020-08-26T13:26:04Z
dc.date.available2020-08-26T13:26:04Z
dc.date.issued1891
dc.identifier.urihttps://hdl.handle.net/11250/2675174
dc.description.abstractForkortet: In the first part of this paper the author describes the solid rocks, beginning with the East. Near the Russian frontier is the Varanger fiord (map.p.26). From the country south of this fiord only stray observations exist. On the northern side are sandstone mountains (illustration p. 23) with bedding in part more or less horizontal; generally, however, the strata is dislocated, as shown by section along the eastern shore on the Tana fiord. Between the Archaean and the younger strata faulting is perhaps the general rule. The small sketch-map p.27 is from a place where this may be clearly seen.
dc.language.isonor
dc.relation.ispartofseriesNGU (4)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectPETROGRAFI
dc.subjectOMDANNET BERGART
dc.subjectKVARTÆRGEOLOGI
dc.subjectSTØRKNINGSBERGART
dc.subjectSEDIMENTÆR BERGART
dc.titleIagttagelser fra en reise i Finmarken 1890
dc.typeJournal article
dc.description.localcode36211
dc.source.pagenumber22-111


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