Blar i Artikler på emneord "AVSETNING"

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    • En undersøkelse av kvartære, økostratigrafiske soner i Drammen, på grunnlag av foraminiferer. 

      Risdal, Dag (NGU (215), Journal article, 1962)
      1. The present paper is a report on a quantitative study of the fossil, benthonic foraminifera of Late- and Post-Galcial clay samples from Drammen, Norway. 2. On the basia of their content of foraminifera, it has been ...

    • Erfaringer om jordskade ved vassdragsreguleringer. 

      Holmsen, Gunnar (NGU (218), Journal article, 1963)
      Prior to the carrying out of the work permitted by a regulation licence, it is the practice in Norway to establish a court of enquiry to investigate the possible economic consequences of damage resulting from regulating. ...

    • Evaluation of sand and gravel in Finnmark as a guide to locating deposits suited to building purposes. 

      Bakkejord, Knut J. (NGU Bulletin (403), Journal article, 1985)
      Forkortet. Bedrock mapping and investigations of rock-types in Finnmark as well as else- where in Norway have made it possible to classify the components by their strength or mechanical properties. Three categories of ...

    • Foraminifera in late quaternary deposits from the Oslofjord area. 

      Feyling-Hanssen, Rolf W. (NGU (225), Journal article, 1964)
      Approximately 2500 core samples from 130 borings, 4 m to 40 m deep, in Late Quaternary (latest Allerød through Sub-Atlantic) clay deposits in the Oslofjord area in southeastern Norway were investigated micropaleontologically. ...

    • Forekomster av tillitt på nordsiden av Atnsjøvinduet, Syd-Norge. 

      Ilebekk, S.; Siedlecka, Anna (NGU (373), Journal article, 1982)
      A previously reported tillite-like conglomerate occurring on the northern side of the Atnsjø Window rests with an erosional contact on Precambrian granite and gabbro and is overthrust by fieldspathic metasandstones of the ...

    • Glacial geology of the area between Jostedalsbreen and Jotunheimen, South Norway. 

      Vorren, Tore O. (NGU (291), Journal article, 1973)
      Ice movement and the course of deglaciation are reconstructed. The age of and the climate during the deglaciation are discussed in the light of equilibrium line displacement, shoreline positions, pollen analysis and ...

    • Glacial geology of Western Troms, North Norway. 

      Andersen, Bjørn G. (NGU (256), Journal article, 1968)
      A moraine chronology was established for western Troms. Altogether six main glacial phases were recognised. Several of the phases were radiocarbon dated. Observations were made of the corresponding shore lines, the marine ...

    • Glidning av Arnebråtveien nr. 30. 

      Holmsen, Gunnar (NGU (166), Journal article, 1946)
      At Arnebråtveien 30 in Aker a sliding of the clayey ground occurred in the evening of May 29th 1936. A road had been built on a foundation of stone. The ground was too weak to stand the weight of the ballast. By a sliding ...

    • Glidning og ras av jernbanefyllinger 16-19 april 1937. 

      Holmsen, Gunnar (NGU (166), Journal article, 1946)
      During these days a remarkable number of slides damaged Norwegian railways. April 16th a sandy railway ballast slid out near Skotselv station between Hokksund and Hønefoss. 5000 m3 of ballast slid into the Drammen river, ...

    • Glimmermineralernes betydning som kalikilde for plantevern 

      Goldschmidt, V.M.; E. Johnson (NGU (108), Journal article, 1922)
      Denne avhandling inneholder en undersøkelse over oppindelsen av jordbundens kaliindhold, eller nærmere præcisert den del av jordbundens kaliindhold som kan tilgodegjøres av planterne.Hittil har man som regel gaat ut fra, ...

    • Gravel fraction on the Spitsbergen Bank, NW Barents Shelf. 

      Edwards, Marc B. (NGU (316), Journal article, 1975)
      The gravel fraction of the bottom sediment on the Spitsbergen Bank, located south of Svalbard in the NW Barents Sea, is composed predominantly of clastic sedimentary rocks, especially sandstone and shale. Betwwen sampling ...

    • Grunnvatnet 

      Rekstad, J. (NGU (92), Journal article, 1922)

    • 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 der existeret store, isdæmmede indsjøer paa østsiden av Langfjeldene? 

      Reusch, Hans (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? 

      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. ...

    • I. Rendalens bræsjø 

      Holmsen, Gunnar (NGU (79), Journal article, 1916)
      The present paper forms a supplement to the author's: Ice-dammed lakes of Northern Østerdal, NGU nr. 73. The lowest sete-building lake in the Glommen valley has extended its branches into the valleys Rendalen, Tydalen and ...

    • 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 ...

    • II. Om isskillet i trakten omkring Fæmund 

      Schiøtz, O.E. (NGU (68), Journal article, 1913)
      Forkortet: As Hørbye first pointed out, the erratic blocks in the region around Femunden show that the ice of E of a line from Sorkvola to Tufsingdal has moved north- wards, while the movement W of that line has been ...

    • 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 ...