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dc.contributor.authorMangerud, Jan
dc.coverage.spatial18174 Fåvang
dc.coverage.spatial17183 Skåbu
dc.coverage.spatial17182 Vinstra
dc.coverage.spatial18183 Ringebu
dc.coverage.spatialNORD-FRON
dc.coverage.spatialSØR-FRON
dc.coverage.spatialRINGEBU
dc.date.accessioned2020-08-26T12:54:45Z
dc.date.available2020-08-26T12:54:45Z
dc.date.issued1963
dc.identifier.urihttps://hdl.handle.net/11250/2674777
dc.description.abstractObserved glacial striae showing direction of ice-movement during the last active stage of the inland-ice are shown in fig. 1. Supposed major directions of ice movement are also shown in fig. 3. In the mountain parts are found a great number of channels connected with the downmelting of the ice. As these meltwater-channels occur close to the highest summits, the latter must have been sityated below the firn-line when they emerged as nunataks above the ice surface. The dead ice mass was wasted by vertical thinning out, the faintly inclined ice tongues gradually retreating from the mountain sides. The orientation and position of the drainage channels have been used in determining the inclination of the ice surface. From the last active stage of the inland ics, shown by glacial striae, the culmination area moved 20-40 km southwards during the stagnant stage.
dc.language.isonor
dc.relation.ispartofseriesNGU (223)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectISAVSMELTING
dc.subjectBREELVAVSETNING
dc.subjectAVSETNING
dc.subjectKARTLEGGING
dc.subjectBREBEVEGELSE
dc.subjectGLASIALGEOLOGI
dc.titleIsavsmelting i og omkring midtre Gudbrandsdalen.
dc.typeJournal article
dc.description.localcode35347
dc.source.pagenumber223-274


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