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Jordfaldet ved Mørset i Stjørdalen.
(NGU (32), Journal article, 1901)Forkortet:The railway from Trondheim to Sweden runs East through the Stjørdal.The lower part of this valley is open and wide. About 9 km from the sea, themain river is joined from the north by the small river Gråelven which ... -
Listerlandet
(NGU (32), Journal article, 1901)Forkortet: The Listaland is a low treeless tract of land at the open sea somewhat to the West of Lindesnes the southernmost promontory of Norway. The Listaland consists of moraine; its boundary line against the mountainous ... -
Geologisk kartskisse over trakterne omkring Velfjorden med beskrivelse
(NGU (34), Journal article, 1901)Forkortet: Velfjorden is situated in northern Norway, in the southern part of the district of Helgeland, in 65\u00B0 30'N. A geological map of the region is given on pp.8 and 9. The eruptive rocks here are granite, gabbro ... -
Geologisk kartskisse over trakterne omkring Velfjorden med beskrivelse. Marmorforekomster
(NGU (34), Journal article, 1901)Forkortet: At Heggefjord, a branch of Velfjorden, marble was formerly quarried, but the work is now suspended. Director J.P.Friis, on pages 30 to 40, has described several localities in this region, containing marble of ... -
Oplysninger til Blakstads jordbundskart over Trondhjems omegn
(NGU (32), Journal article, 1901)Forkortet: Most of the area represented on the map consists of marine clay which is left white on the map p.113. The finely striated parts are sandy clay and the finely dotted parts are sand. River gravel is designated ... -
Høifjeldet mellem Vangsmjøsen og Tisleia (Valdres)
(NGU (32), Journal article, 1901)Forkortet: This region lies in the midst of Southern Norway to the NNW of Oslo. The Valdres valley, shown on the maps, pp.86 and 87 stretches from the Vangsmjøs in the NW the Strandefjord in the SE. The bottom of this ... -
En forekomst af kaolin og ildfast ler ved Dydland nær Flekkefjord
(NGU (32), Journal article, 1901)Forkortet: The lower part of the Sire river in Southwestern Norway has the appearance of a fjord 4 km long. Not far from it is Jøsingfjord only 2 km long. The peninsula between these two fjords is as a whole rather low and ... -
Nogle bidrag til forstaaelsen af, hvorledes Norges dale og fjelde er blevne til
(NGU (32), Journal article, 1901)Forkortet: Up to the present, the relief of Norway has not been understood sufficiently to allow of a satisfactory explanation being given of even the most salient features, such as the contrast between plateau and valley, ... -
Nogle optegnelser fra Værdalen
(NGU (32), Journal article, 1901)Forkortet: About 12.30 A.M. on the 19th May 1893 occurred the great landslip in Verdal which had the effect of concentrating the attention to the whole country upon that valley for several weeks. The little sketch map ... -
Skjærgaarden ved Bergen
(NGU (32), Journal article, 1901)Forkortet: Maps of the region described are given on pp.106 and 107. The second forms a continuation to the South of the first. The parallel og 60\u00B0 30' N goes over the tract. The area belongs to the coastal plain, ... -
Iagttagelser fra bræer i Sogn og Fjordane
(NGU (34), Journal article, 1901)Forkortet: In the valleys in front of the Norwegian glaciers, there are nearly always great plains of sand and gravel, which the glacial streams have deposited. Om pp. 4 to 8, this is instanced by an account of the fluvial ... -
Etage 5 i Asker ved Kristiania. Studier over den norske Mellemsilur
(NGU (34), Journal article, 1901)Forkortet: The present work gives the results of the author's researches in the Middle Silurian (Stage 5) in Asker, which lies nearly 10 miles SW from Oslo, on the west side of the head of the Oslofjord. In the first place ... -
En notis om istidsgruset ved Lysefjordens munding
(NGU (32), Journal article, 1901)Forkortet: The mouth of the Lysefjord is situated at 58\u00B0 52' n.l. to the SE of the town of Stavanger. The glacial deposits here are of interests in the history of geology Esmark found as far back as 1824 at this place ... -
Aarbog for 1900
(NGU (32), Journal article, 1901)Nogle optegnelser fra Værdalen av Hans Reusch. Jordfaldet ved Mørset i Stjørdalen av Hans Reusch. Høifjeldet mellem Vangsmjøsen of Tisleia (Valdres) av Hans Reusch. Listerlandet av Hans Reusch. En notis om istidsgruset ved ... -
Nogle optegnelser fra Andøen
(NGU (36), Journal article, 1902)Forkortet: Appendix, by Dr. Reusch. At the Southern border of the coal field one finds, that the Jurassic deposits are separated from the Archæan by faultlines. Studies of the rocks both in the solid parts and in the loose ... -
Fra det indre af Finmarken
(NGU (36), Journal article, 1902)Forkortet: The solid rock. In the region between Bjørnstad (NW corner of the map) and the first geological boundary line (dotted on the map) there are mostly sheared, quartzitic, feldsparbearing sandstone, lying more or ... -
Fra Hardangervidden II
(NGU (34), Journal article, 1902)Forkortet: The present author has chiefly worked in the middle part of the district. The sections on p.37 show granitic rocks that have been pushed over the Cambro- Silurian phyllite along thrust-planes. The picture on ... -
Geologisk litteratur vedkommende Norge 1896-1900
(NGU (33), Journal article, 1902) -
Fra Hardangervidden III
(NGU (34), Journal article, 1902)Forkortet: The border-lines on the southwestern and southern part of the map on p.29 are to be attributed to Mr.Bjørlykke, who had a very wild region to explore. His photo, reproduced on p.63, shows veins of granite in ... -
Fra Hardangervidden I
(NGU (34), Journal article, 1902)Forkortet: The map on p.29 shows the chief geological divisions. Brøgger has found that the succession of strata in the Hårteigen Mountain has been as follows. 1. Lowermost, lying on old granite, Alum-schist (in Hulberget ...