dc.contributor.author | Reusch, Hans | |
dc.coverage.spatial | 23353 Varangerbotn | |
dc.coverage.spatial | 23352 Nesseby | |
dc.date.accessioned | 2020-08-26T12:32:55Z | |
dc.date.available | 2020-08-26T12:32:55Z | |
dc.date.issued | 1891 | |
dc.identifier.uri | https://hdl.handle.net/11250/2674462 | |
dc.description.abstract | Forkortet: The uppermost Fig. on p.79 shows the low mountains on the north side of the inner part of the Varangerfjord not far from the Russian border. At b and x occurs a little schist. The rest of the moountains consists of conglomerate at least 50 m thick. The conglomerate (the second fig. on p.79) shows no trace of stratification. It is a redish claybearing sandstone filled with stones attain- ing the size of a head or more. The big stones are rather few. The stones are mostly of Archaean origin, gneiss and granite; also dioritic rocks occur; dolomite and pure quartz are found comparatively seldom. The stones have not the habitus of water-worn rolling-stones. The conglomerate has quite the appearance of boulder-clay. It was therefore very inviting to search for stri- ated stones. The search was at first not successful; only some small slickensides in the groundmass and on some surface of the boulders were found. The slickensides were covered with a chloritic substance. | |
dc.language.iso | nor | |
dc.relation.ispartofseries | NGU (1) | |
dc.rights | Navngivelse 4.0 Internasjonal | |
dc.rights.uri | http://creativecommons.org/licenses/by/4.0/deed.no | |
dc.subject | PETROGRAFI | |
dc.subject | SEDIMENTÆR BERGART | |
dc.subject | SANDSTEIN | |
dc.subject | BREBEVEGELSE | |
dc.subject | KONGLOMERAT | |
dc.title | Skuringsmærker og morænegrus eftervist i Finmarken fra en periode meget ældre end "istiden" | |
dc.type | Journal article | |
dc.description.localcode | 36248 | |
dc.source.pagenumber | 78-85 | |