• C14-datings referring to shore lines, transgressions, and glacial substages in Northern Norway. (A supplement to papers of 1960 and 1961 by the author). 

      Marthinussen, M. (NGU (215), Journal article, 1962)
      Denne publikasjonen er en foreløpig meddelelse som i det vesentlige dreier seg om en serie C14-dateringer utført av R. Nydal ved Laboratoriet for Radiologisk Datering i Trondheim. Dateringene synes å gi viktige opplysninger ...
    • 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 ...
    • 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 ...
    • 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 ...
    • 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 ...
    • Micropaleontology applied to soil mechanics in Norway. Mikropaleontologi anvendt på geotekniske problemer i Norge. 

      Feyling-Hanssen, R.W. (NGU (197), Journal article, 1957)
      A breif review of the geological history of the Late Pleistocene marine clay deposits of the Oslofjord area, southeastern part of Norway, has been given, and a stratigraphical division of these sediments, established upon ...
    • Mikropaleontologiens teknikk. 

      Feyling-Hanssen, Rolf W. (NGU (203), Journal article, 1958)
      Technique of micropaleontology: The article describes the treatment of Formanifera samples from Norwegian Late Pleistocene marine clays. The samples is collected with a thin-wall, stationary piston samper with entrance ...
    • 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 ...
    • 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 ...
    • Om de senglaciale og postglaciale nivåforandringer i Kristianiafeltet (Molluskfaunaen). 

      Brøgger, Wilhelm C.; Med bidrag av E.B.Munster, P.Øyen o.fl. (NGU (31), Journal article, 1900)
      Forkortet:The great terminal moraine ridges - the ra's - on both sides of the Oslo Fjord were formerly, especially by De Geer, commonly supposed to indicate the uttermost limit of the last great ice sheet; on pp.3-8 it is ...
    • Om faunaen i nogle skjælbanker og lerlag ved Norges nordlige kyst 

      Holmboe, Jens (NGU (37), Journal article, 1903)
      Forkortet: While a high-arctic climate vet was prevailing, a submergence seems to have taken place in the north of Norway, corresponding to the late glacial sub- mergence at the Oslofjord, according to Brøgger's investigations. ...
    • Om norske jordarters variasjon i korngradering og plastisitet. 

      Selmer-Olsen, Rolf (NGU (186), Journal article, 1954)
      This paper presents the final results of an investigation on plasticity and grain size distribution in Norwegian soils. A part of the results has been summarized in \"Proceedings of the Third International Conference on ...
    • Oppland. Beskrivelse til kvartærgeologisk landgeneralkart. 

      Holmsen, Gunnar (NGU (187), Journal article, 1954)
      The present map of the quaternary deposits of Oppland was prepared on the general principles applied to the preceding map of Oslo and outlined in the accompanying publication, NGU no. 176. As the ice front retired and the ...
    • Oslo. Beskrivelse til kvartærgeologisk landgeneralkart. 

      Holmsen, Gunnar (NGU (176), Journal article, 1951)
      Marine deposits: All along the coast of Norway above the present sea level there are raised beaches, caves and terraces formed by waves. This proves that formerly the ocean reached a higher level. The highest one since the ...
    • Statsgeologenes årsberetninger for 1923. Skjellbanker i Lørenskog. 

      Rekstad, J. (NGU (122), Journal article, 1924)
    • Terrænundersøgelser og jordboringer i Stjørdalen, Værdalen og Guldalen samt i Trondhjem i 1894, 95 og 96 

      Friis, Jacob P. (NGU (27), Journal article, 1898)
      Forkortet: The Norwegian valleys filled up at a large extent by gravel, sand and clay in the course of time been submitted to earthslips and sinking of the grounds, however more especially those of Gauldalen, Stjørdalen ...