Browsing Artikler by Title
Now showing items 369-388 of 1064
-
Hallingdal. Beskrivelse til kvartærgeologisk landgeneralkart.
(NGU (190), Journal article, 1955)(forkortet): The present map of the quaternary deposits of Hallingdal was prepared on the general principles reffered to in the summary of Oslo, NGU no. 16, the first map description published in this series and followed ... -
Hans Reusch. Nekrolog og bibliografi
(NGU (100), Journal article, 1923)The present publication is dedicated to the memory of Dr. Hans H. Reusch,\r late director of the Norwegian Geological Survey. It also contains a\r bibliography of books, papers, and articles published by Dr. Reusch.\r Dr. ... -
Har der existeret store, isdæmmede indsjøer paa østsiden av Langfjeldene?
(NGU (14), Journal article, 1894)Langfjeldene is the great mountainridge, which runs through southern Norway. Mr.Andr.M.Hansen have forwarded the hypothesis, that in the region east of it (map p. 52) there existed at the end of the ice-age large lakes ... -
Har Jæren vært dekket av en Skagerak-bre? Er "Skagerak-morenen" en marin leire?
(NGU (228), Journal article, 1964)Jæren is a low plain on the coast of southwestern Norway. This plain is covered with relatively thick Quaternary deposits including a very bouldary W\u00CFrm till on top of calcareous clays and stratified sand and gravel. ... -
Harstad. Beskrivelse til det berggrunnsgeologiske gradteigskart M 8 - 1:100 000 (med fargetrykt kart)
(NGU; Skrifter (309; 14), Journal article, 1974)From a structural point of view the bedrocks of the map area can be subdivided into 1. Precambrian basement (autochthonous), and 2. Allochthonous Caledonian units. The Caledonian sequence embraces a) The lowermost over-thrust ... -
Håfjellsmulden i Ofoten og dens sedimentære jern-mangan-malmer. Søndre Ofotens malmforekomster II.
(NGU (174), Journal article, 1949)The sedimentary hematite-magnetite ores of marine origin, occurring within the crystalline mica schists of the caledonian mountain of Northern Norway, belong to a characteristic type of iron ore deposits, internationally ... -
Heavy-mineral provinces in southern Skagerrak and northern Kattegat
(NGU Bulletin (430), Journal article, 1996)Detailed heavy-mineral studies of the bottom sediment in the Skagerrak-Kattegat area have not been previously reorted. The heavy-mineral suite in the very- fine-sand fraction (63-125um) is dominated (70-91%) by amphibole, ... -
Hellemobotn og Linnajavrre. Geologisk beskrivelse til kartbladene.
(NGU (150), Journal article, 1942)The situation of the maps is shown on p. 6. They form the southern continuation of the map Tysfjord, recently described by the author (NGU no. 149). The petrology and chemistry of the rocks are reserved for a special paper. ... -
Hemsedal og Gol. Beskrivelse til de geologiske gradteigskarter E32V og E32Ø.
(NGU (153), Journal article, 1939)The two accompanying maps cover a territory in the central part of Norway, between Hallingdal and Valdres. The district is built up of Caledonian highland formations and highland eruptives covering the sedimentary formations. ... -
High-temperature ultramafic complexes in the North Norwegian Caledonides: I - Regional setting and field relationships.
(NGU Bulletin (405), Journal article, 1986)Forkortet.Four major (25-100 km\u00B2) ultramafic complexes were developed in the Sørøy Nappeduring the second phase of Finnmarkian deformation in the North NorwegianCaledonides. They were emplaced into layered mafic ... -
Hosanger nikkelgruve.
(NGU (172), Journal article, 1949)(forkortet) The Hosanger nickel deposits are situated on the western coast of southern Norway, about 20 km NE of Bergen. Nickel ore has been produced in 4 mines, Nonås, Litland, Lien I, Lien II Smith Meyers mine). The ... -
Huse af granit
(NGU (1), Journal article, 1891)Forkortet. Houses of granite. The Scottish manner of building is not unsuitable for Norway. -
Hydrogeological investigation of water for export from Nordland county, Norway
(NGU Bulletin (427), Journal article, 1995) -
Hydrogeology in the Romerike area, southern Norway
(NGU Bulletin (418), Journal article, 1990)A hydrogeological model has been developed on the basis of field observat- ions and data collected during the International Hydrological Decade. From water balance studies it was found that half the annual precipitation ... -
Hyolithus-sonens basale lag i Vest-Finnmark.
(NGU (195), Journal article, 1956)The basal layers of the \"Hyolithus-zone\" in western Finnmark: The \"Hyolithus- zone\" is a term which has been attached to the autochtonous Cambrian substratum of the Caledonides which can be followed from Laksefjord in ... -
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 ... -
Høifjeldskvartsens nordøstligste udbredelse
(NGU (14), Journal article, 1894)The region treated of in this paper lies to the Northeast of the region described by Reusch in his paper: The region between Bygdin and Bang. Kjerulf has divided the sedimentary strata in central Norway is sparagmite ... -
I. Den hvite granit i Sogn, geologisk optræden og tekniske egenskaper
(NGU (68), Journal article, 1913)Forkortet: The white granite of Sogn in Western Norway, although for many years known and repeately called attention to be geologists, has only recently come into use as a building material to any extent. In this paper is ... -
I. Fjeldstrøket mellem Lyster og Bøverdalen
(NGU (69), Journal article, 1914)Forkortet: The tract of land here treated is situated in Southern Norway between Sogne- fjord and Bøverdal, at 61\u00B030'N and at 3\u00B0W of Oslo. The rocks of the region form the following sections: 1. Archaean gneiss ... -
I. Fra indre Helgeland. Fjeldbygningen og bergartene samt bemerkninger om bergverksdriften
(NGU (59), Journal article, 1911)Forkortet: Helgeland, the southern part of the district of Nordland, it situated between about 65\u00B0 and 66 1\/2\u00B0 N. Some of the inner parts of this great district were the object of the author's investigations ...