Browsing Artikler by Subject "KVARTÆRGEOLOGI"

Now showing items 1-20 of 73

    • A buried late MIS 3 shoreline in northern Norway - implications for ice extent and volume 

      Olsen, Lars (NGU Bulletin (450), Journal article, 2010)
      Buried beach gravel in northern Norway represents a late Middle Weichselian\/Marine Isotope Stage (MIS) 3 shoreline and indicates a significant late MIS 3 ice retreat. An age of c. 50-31 cal ka BP, or most likely c. 35-33 ...

    • Aarbog for 1894 og 95 

      Reusch, Hans (NGU (21), Journal article, 1896)

    • Age of the Younger Dryas ice-marginal substages in Mid-Norway - Tautra and Hoklingen, based on a compilation of 14C-dates 

      Olsen, Lars; Sveian, Harald; Høgaas, Fredrik (NGU Bulletin (454), Journal article, 2015)
      The ice-marginal Tautra and Hoklingen Substages in the Trøndelag counties, Mid-Norway, have for a long time been referred to as of early and late Younger Dryas (YD) age, respectively. The basis for this is the regional ...

    • Beskrivelse til kartbladet Dønna 

      Rekstad, Johan (NGU (37), Journal article, 1904)
      Forkortet: This region is situated in the Northern part of the district of Helgeland between 66\u00B0 and 66\u00B0 20' N. A geological map in black is given on pages 4 and 5. The igneous rocks here are granites, gabbro and ...

    • Bidrag til Finmarkens geologi 

      Holtedahl, Olaf (NGU (84), Journal article, 1918)
      The present paper is a result of investigations carried out in the most northern district of Norway, during the summers 1914-17, the total amount of time spent in Finnmark being 23 weeks. The studies have been confined to ...

    • Børgefjell. Beskrivelse til det berggrunnsgologiske gradteigskart J.19 - 1: 100 000 

      Gustavson, Magne (NGU; Skrifter (298 ; 8), Journal article, 1973)
      Three main structural units are present: 1. The Precambrian (Svecofennokarelian) basement of the Børgefjell Window. \". Low grade (greenschist facies) Lower Paleozoic rocks belonging to the Seve-Køli Nappe Complex. 3. The ...

    • Code of stratigraphic nomenclature for Norway 

      Bjørlykke, Harald (NGU (213), Journal article, 1961)

    • Distribution of rock fragments, grain size and chemical elements of tills in the Lake Mjøsa area, eastern Norway 

      Reimann, Clemens; Olsen, Lars; Fredin, Ola; Follestad, Bjørn A. (NGU Bulletin (453), Journal article, 2014)
      The Lake Mjøsa area in eastern Norway forms an interesting case to study glacial erosion, transport and deposition because bedrock lithology (source of till) is relatively well known and the Geological Survey of Norway ...

    • Dunderlandsdalen. Fjeldbygningen inden gradavdelingskartet Dunderlandsdalens omraade 

      Oxaal, John (NGU (86), Journal article, 1919)
      This paper is a geological description of the Dunderland district in Nordland, a part of Northern Norway. The map accompanying the paper is a part of the official series of maps on the scale of 1:100 000, which is being ...

    • Egersund. Fjeldbygningen inden rektangelkartet Egersunds omraade 

      Kolderup, Carl Fredrik (NGU (71), Journal article, 1914)
      Forkortet: The principal part of the rocky underground consists of labradorite-rocks, as may be seen on the map. These are not homogeneous all over the area neither with regard to the mineralogical composition, nor regarding ...

    • En geologisk undersøkelse på den nordvestlige del av kartblad Børgefjell. 

      Gustavson, Magne; Grønhaug, Arne (NGU (211), Journal article, 1960)
      A geological investigation of the Caledonid of the Majavatn-Kvigtindregion, Nordland, Norway. The northwestern part of the map area Børgefjell, Nordland, was investigated during the summers of 1957 and 1958, seven weeks ...

    • En geologisk undersøkelse på den sørøstre del av kartbladet Salangen. 

      Lund, Per Ragnar (NGU (234), Journal article, 1965)
      Petrographic and structural investigations were made in a Cambro-Ordovician area of the Caledonides of Northern Norway, situated in Salangen, Troms. The rocks, mainly mica schists rich in biotite and\/or muscovite, are ...

    • Fjeldstrøget mellem Saldalen og Dunderlandsdalen. 

      Rekstad, Johan (NGU (67), Journal article, 1913)
      Forkortet:The region described is situated in the interior of Northern Norway between66\u00B0 30' and 67\u00B0N, and to the east of the Territory treated in The Geology ofNorthern Helgeland, NGU Nr.62.The stratified rocks, ...

    • Fortsetter Horrsjøbergets sedimentserie inn i Norge? 

      Bryn, Knut Ørn (NGU (215), Journal article, 1962)
      An erratic quartizitic boulder, rich in kyanite, was found at Storsjøen, N. Odal, Southern Norway. The boulder also contains lazulite, rutile, pyrite and svanbergite. Lazulite and svanbergite have not been reported from ...

    • Fotogeologi 

      Siggerud, Thor (NGU (205), Journal article, 1959)
      The use of air photos for geological interpretation is described. A short introduction to photogrammetry is given, and the types of instruments useful for photogeology are mentioned.

    • Four sediment cores from the Continental Shelf outside Trøndelag. 

      Haldorsen, Sylvi (NGU (304), Journal article, 1974)
      Grain size analysis and clay mineral investigations have been carried out. The cores consist of an assemblage of sand, silt and clay, where the clay content is gradually decreasing from the bottom towards the top of the ...

    • Fra det indre af Finmarken 

      Reusch, Hans (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 det nordøstlige af Jotunfjeldene 

      Rekstad, Johan (NGU (37), Journal article, 1904)
      Forkortet: This mountain region forms the highest part of Southern Norway between latitudes 61\u00B0 28' and 61\u00B0 46' N. The two highest mountains in Norway, Gald- høpiggen and Glittertinden, lie within the territory. ...

    • Fra Hardangervidden I 

      Reusch, Hans (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 ...

    • Fra høifjeldsstrøget mellem Haukeli og Hemsedalsfjeldene 

      Rekstad, Johan (NGU (36), Journal article, 1903)
      Foredrag: This mountainous region is situated between latitudes 59\u00B0 50' and 61\u00B0 N in the highest parts of the country. In 1900 Reusch, Bjørlykke and the writer surveyed the western and southern parts of this ...