Blar i Artikler på emneord "BREELVAVSETNING"

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    • De fem jordartsregioner i Norge. 

      Holmsen, Gunnar (NGU (195), Journal article, 1956)
      The five soil regions of Norway: The greater part of the deposits covering the rock in Norway were placed in their present position during the melting period of the inland ice. In studying the formation of soils two different ...

    • Einergrein av Preboreal alder funnet i israndavsetning i Eidfjord, Vest-Norge. 

      Rye, Noralf (NGU (266), Journal article, 1970)
      In 1969 a branch of juniper (Juniperus communis) was found in a sand-pit on the ice marginal delta in Eidfjord, West-Norway. Radiocarbon dating gave an age of 9680\u00B190 years B.P., which means that the delta is Preboreal ...

    • En "flyttblokk" av finsand. 

      Låg, J. (NGU (255), Journal article, 1968)
      An \"erratic boulder\" of fine sand: A special, isolated deposit of fine sand in a coarse sand deposit of fluvio-glacial character at Brusletten, Dovre, in central Norway has been described. The fine sand has probably been ...

    • En notis om istidsgruset ved Lysefjordens munding 

      Reusch, Hans (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 ...

    • Hallingdal. Beskrivelse til kvartærgeologisk landgeneralkart. 

      Holmsen, Gunnar (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 ...

    • Har Jæren vært dekket av en Skagerak-bre? Er "Skagerak-morenen" en marin leire? 

      Andersen, Bjørn G. (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. ...

    • Iagttagelser fra bræer i Sogn og Fjordane 

      Rekstad, Johan (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 ...

    • 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 ...

    • 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 ...

    • Jordartregioner i Norge. 

      Holmsen, Gunnar (NGU (213), Journal article, 1961)
      As older geological maps mainly present bedrock geology to the neglect of drift, the Geological Survey of Norway (NGU) year 1936 realized the need of a special map to supply necessary information about quaternary deposits. ...

    • Jæderens jordbund. 

      Grimnes, A. (NGU (52), Journal article, 1910)
      Forkortet:The comparatively flat extent of country which stretches from the neighbour-hood of Stavanger to the neighbourhood of Vigrestad, has above the bed-rocka cover of loose material which in the southern part attains ...

    • 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 ...

    • Listerlandet 

      Reusch, Hans (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 ...

    • 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 ...

    • 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 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. ...

    • Norske kilder. Meddelelse fra Vannboringsarkivet nr. 7. 

      Skjeseth, Steinar (NGU (203), Journal article, 1958)
      Norwegian springs may be divided into two main groups: A. Springs from Quaternary deposits. B. Springs from rock. Common types of springs from Quaternary deposits are shown in figs. 1-3. In areas covered by sea, during and ...

    • 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 ...

    • Nyttbare sand- og grusforekomster i Syd-Norge. Del II: Grustakenes art og beliggenhet. 

      Holmsen, Gunnar (NGU (271), Journal article, 1971)

    • 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 ...