Blar i Artikler på emneord "AVSETNING"

Viser treff 41-60 av 137

    • 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 ...

    • Jomaforekomstenes blokkvifter. 

      Oftedahl, Christoffer (NGU (200), Journal article, 1957)
      The Joma pyrite occurence contains some 15 million tons ore and crops out mostly under bogs with maximum ore zonewidth of 40 m. The surrounding morainic deposits have been investigated for ore boulders, in order to find ...

    • 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. ...

    • Jordfaldet ved Mørset i Stjørdalen. 

      Reusch, Hans (NGU (32), Journal article, 1901)
      Forkortet:The railway from Trondheim to Sweden runs East through the Stjørdal.The lower part of this valley is open and wide. About 9 km from the sea, themain river is joined from the north by the small river Gråelven which ...

    • Jæderens geologi. 

      Bjørlykke, Knut O. (NGU (48), Journal article, 1908)
      Forkortet:Jæren is the comparatively flat district on the South Western coast of Norway,between Stavanger and Egersund. The soil consists in most parts, of deposits ofloose material, moraine sand and gravel, peat moss and ...

    • 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 ...

    • 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 Proterozoic (Vendian) to Early Cambrian sedimentation in the Hedmark Group, south-western part of the Sparagmite Region, southern Norway 

      Dreyer, Tom (NGU Bulletin (412), Journal article, 1988)
      Field studies of the allochthonous Ekre Shale and Vangsås Formation (uppermost Hedmark Group) were undertaken in order to develop a sedimentary model for the final stages of infilling of the Hedmark rift basin. The Ekre ...

    • Leirfall på Nedremule, Byneset 1943. 

      Holmsen, Gunnar (NGU (167), Journal article, 1946)
      At Nedre Mule in Byneset about 20 km west of Trondheim, a clay slide occurred on the 24th of May 1943, wasting 20 000 sq. m. of cultivated land. The ground slid into the fjord Gulosen. A mud flow was visible in the course ...

    • Leirfall ved Aaserumvatnet i Hedrum 1940. 

      Holmsen, Gunnar (NGU (167), Journal article, 1946)
      On the first of July 1940 a clay-slide took place on the beach of lake Aaserumvatnet, 10 km West of Sandefjord. The slide occurred in several repetitions. Commencing at 7 o'clock in the morning the ground was not at rest ...

    • Leirfall ved Holund i Grong 1942. 

      Holmsen, Per (NGU (167), Journal article, 1946)
      On january 19th, 1942 a violent clay-slide took place near the farm Holund in Grong district, east of Namsos. The size of the displaced area was about 1 acre. A heavy wave of liquid clay rushed down into a small valley. ...

    • Leirfall ved Kulstadsjøen, Vefsnfjorden 1940. 

      Holmsen, Gunnar (NGU (167), Journal article, 1946)
      During the building of the railway line between Mosjøen and Mo in Nordland, the nearly completed work on the ballast was destroyed by a submarine slide on August 31th, 1940. The railway line 3 km north of Mosjøen along the ...

    • Leirfall ved Leirnesset, Foldereid 1939-40. 

      Holmsen, Per (NGU (167), Journal article, 1946)
      In the autumn of 1930 a clay-slide took place near Foldereid, Northern Norway. Part of the cross country road to Nordland was touched by the slide. In order to reconstruct the road traverse, borings and ground studies were ...

    • Leirfallet ved Knivsvik i Hurum 1940. 

      Holmsen, Per (NGU (167), Journal article, 1946)
      In the night preceding to October 11th, 1940, a clay-slide took place by Knivsvik near Drammen. This was a typical clay-slide; some liquid clay (\"Kvikkleire\") flowed down a brooklet called Knivsvikbekken. Most of the ...

    • Leirfallet ved Kverne i Stokke 1944. 

      Holmsen, Gunnar (NGU (167), Journal article, 1946)
      In a marine clay deposit at Kverne in Stokke, near the town of Tønsberg, a great fall of the ground took place on Oct. 9th, 1944. The area hit by the slide amounts to 76 500 sq. metres of well cultivated field. Through a ...

    • Leirfallet ved Lade, Trondheim 1944. Foredrag holdt i Norsk Geologisk Forening 11.4.1945 

      Holmsen, Per (NGU (167), Journal article, 1946)
      On April 11. 1944 a clay-slide took place near Ladehammeren N of Trondheim. About 5 acres of the field between Lade Alle and the Ladebekken streamlet slid down. Liquid clay was not visible. There was great uncertainty about ...

    • Lerfaldene ved Kokstad, Gretnes og Braa. 

      Holmsen, Gunnar (NGU (132), Journal article, 1929)
      The marine clay deposits in the South Eastern part of Norway, in the Trondheim district, and in certain valleys in Northern Norway are often distressed by landslides which make freat damages. In historical times the largest ...

    • Lerfall i årene 1930-1932. 

      Holmsen, Gunnar (NGU (140), Journal article, 1934)
      A previous paper (NGU, no. 132) by the same author treats of three recent landslips in marine clay deposits. In the present publication is given a description of some clayslides, which took place in the above mentioned ...

    • Lerfall på eiendommen Solbakken i Sandar. 

      Holmsen, Gunnar (NGU (166), Journal article, 1946)
      This place is situated 1 km North West of the town Sandefjord. In Dec. 1934 a small landslip broke a slope along a rivulet. The wasted area amounted to 1000 sq. m. In the spring of the next year another slip occurred. In ...