Blar i Artikler på emneord "GLASIALGEOLOGI"

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    • Isavsmelting i og omkring midtre Gudbrandsdalen. 

      Mangerud, Jan (NGU (223), Journal article, 1963)
      Observed 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 ...

    • Isfrie refugier i Norge under istiden. 

      Mangerud, Jan (NGU; Skrifter (297; 7), Journal article, 1973)
      A review is given of the historical development of the theory of unglaciated refugia in Norway. The phyto-geographical and geological arguments for and against the theory are discussed, and our knowledge of the ice-borders ...

    • Isrand-dannelser ved Atnesjøen. 

      Werenskiold, W. (NGU (183), Journal article, 1952)
      Atnesjø is a lake in Central Norway, 700 m above sea level just to the SE of the Rondane mountain group. The Atnariver enters the lake from the north, and leaves at the north end, forming an affluent to the great Glomma ...

    • IV. Litt om Jutulhugget 

      Reusch, Hans (NGU (79), Journal article, 1917)
      The Jutulhug (\"The big Troll's Notch\") is a cleft or canyon situated in the central part of Southern Norway under 62 degrees N. As our somewhat schematic drawing on p. 4 shows, it is situated in a wide saddle between the ...

    • Kvartære avleiringer i Østfold 

      Rekstad, J. (NGU (91), Journal article, 1922)
      This paper is a contribution to the quaternary geolgoy of the south-eastern part of Norway. The district lies between the Oslo Fjord and the Swedish frontier. The map, fig. 1 shows the direction of the movement of ice ...

    • Kvartærgeologiske undersøkelser i Randsverkområdet, Jotunheimen. 

      Jørgensen, Per (NGU (228), Journal article, 1964)
      A short account is given of the Late Pleistocene deglaciation and drainage in an area of Jotunheimen (fig. 2). Already at the beginning the mountain tops emerges through the ice sheet, and it is possible to follow the ...

    • Late Precambrian and Cambro-Ordovician sedimentation in East Finnmark. 

      Hobday, D.A.; Reading, H.G.; Banks, N. L.; Edwards, M.B.; Geddes, W.P. (NGU (269), Journal article, 1971)
      The presence of two closely spaced tillite formations within the Precambrian and Cambro-Ordovician sediments of eastern Finnmark permits subdivision into pre-glacial and post-glacial regimes. On the northern side of ...

    • Ljørdalen. Beskrivelse til kvartærgeologisk landgeneralkart. 

      Holmsen, Gunnar (NGU (206), Journal article, 1958)
      The area is characterized by the melting in situ of stagnant glaciers. The glacial material of scree and stream deposits date from the dead-ice stage of the inland ice during which it left eskers of more or less sorted ...

    • Lokalglaciasjon på Sunnmøre. (On the mountain glaciation of Sunnmøre, West-Norway.) 

      Reite, Arne J. (NGU (247), Journal article, 1967)
      Terminal moraines deposited by cirque glaciers are described from Sunnmøre, West Norway. Radiocarbon dating indicates that the fjord districts were free from inland ice in Allerød time. The mountain glaciation most likely ...

    • Løsmateriale og isavsmeltning i nedre Gudbrandsdalen og Gausdal. 

      Bergersen, Ole Fredrik (NGU (228), Journal article, 1964)
      In the present paper are published some preliminary results of a study on glacigene material in two strongly glaciated valleys in Central Norway, namely Gudbrandsdalen and Gausdal. Particular attention has been paid to ...

    • Methods and stratigraphies used to reconstruct Mid- and Late Weichselian palaeoenvironmental and palaeoclimatic changes in Norway. 

      Olsen, Lars; Grøsfjeld, Kari; Stokland, Øystein; Lauritzen, Stein-Erik; Selvik, Synøve F.; Bergstrøm, Bjørn; Sveian, Harald (NGU Bulletin (438), Journal article, 2001)
      A review is presented on the comprehensive stratigraphic database and the methods used for palaeoclimatic and palaeoenvironmental interpretations in Norway during the Mid- to Late Weichselian time interval. The reconstructions ...

    • Moraines in the Hemnefjord area, Western Norway. 

      Lasca, N.P. (NGU (266), Journal article, 1970)
      Four radiocarbon dates are used to date moraines in the inner Hemnefjord area. The radiometric ages of moraines range from approximately 10,720 to 11,310 years B.P. and probably correlate with the Ra moraines in Southern ...

    • Noen glasifluviale isrand-avsetninger i den sydlige del av Glomma- vassdragets (nåværende) dreneringsområde. Med en del berggeologisk-morfologiske data fra de nordlige Øyeren-traktene. 

      Holtedahl, Olaf (NGU; Skrifter (306; 11), Journal article, 1974)
      The present paper represents more or less a continuation of the writer's publication from 1924, which mainly dealt with the northern Romerike district of southeastern Norway, from Jessheim to Lake MjThe present paper ...

    • Noen isavsmeltningsfenomener i Østerdalen. 

      Oftedahl, Chr. (NGU (188), Journal article, 1954)
      Some features from the melting of the inland ice in Østerdalen: A few of the more large-scale features formed by melting water of the last ice sheet are described. The last part of the inland ice filled the valleys in the ...

    • Noen kvartærgeologiske iakttagelser i Lakselvdalen, Finnmark. 

      Skålvoll, Harald (NGU (211), Journal article, 1960)
      Some observations of quaternary deposits in Lakselvdalen, Finnmark: Glacial striae and erratics show that the ice has moved from south to north. Ground moraine, dead ice moraine, marine and glacial-fluvial deposits occur. ...

    • Norges kvartærgeologi. En oversigt. 

      Bjørlykke, K.O. (NGU (65), Journal article, 1913)
      Forkortet:The first part contains an historical survey of the works of the Norwegianquaternary geologists in somewhat chronological order, commencing withJens Esmark (1763-1839), who as early as 1824 described the first ...

    • Nyttbare sand- og grusforekomster i Syd-Norge. Del I: De geologiske betingelser for deres avsetning. 

      Holmsen, Gunnar (NGU (233), Journal article, 1965)
      The transport and deposition of gravel by glaciers and byglacier-fed streams during the deglaciation, have been principallyresponsible for the types of Quaternary deposits found in our country.This process is described in ...

    • Om elve-erosjon og en isdemt sjø i Birtavarre-området, Troms. 

      Dons, Johannes A. (NGU (184), Journal article, 1953)
      The geological survey in the Birtavarre region during the summer 1952 had as its main purpose the investigation of the copper ores of the district. However, some attention was also paid to geomorphological and quaternary ...

    • Om glasiasjonssentra i Sør-Norge under slutten av istiden. En sammenligning mellom et østlig og et vestlig område. 

      Holmsen, Per (NGU (228), Journal article, 1964)
      The traditional study of glacial transport has recently been resumed by the Geological Survey of Norway. Two areas of particular interest have been selected for a comparative study, one around Røros in the East and the ...

    • Oplysninger til Blakstads jordbundskart over Trondhjems omegn 

      Reusch, Hans (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 ...