Blar i Artikler på emneord "KLIMA"

Viser treff 1-9 av 9

    • A 6-ka climatic cycle during at least the last 50,000 years. 

      Olsen, Lars; Hammer, Øyvind (NGU Bulletin (445), Journal article, 2005)
      The distribution of 264 dates in the interval 12,000-50,000 years BP from terrestrial and raised marine sediments from ic-free intervals in Norway shows a fairly strong cycle with a period of c.6 thousand years. The cycle, ...

    • Eemian and Weichselian deposits at Bø on Karmøy, SW Norway: a preliminary report. 

      Andersen, Bjørn G.; Kirkhus, Øyvind; Sejrup, Hans Petter (NGU (380), Journal article, 1983)
      Lithological and biostratigraphical studies, including studies of pollen, foraminifera and molluscs, together with amino acid analysis, radiocarbon datings and Uranium-Thorium datings of the deposits in a 21 m section with ...

    • Et pollendiagram fra Høydalsmo, Telemark. 

      Larssen, Kari Egede (NGU (213), Journal article, 1961)
      In 1959 an elk-horn was found in a bog in Høydalsmo, Lårdal, Telemark, about 580 m above sea level. The finder, Gunnar Aalandslid, collected samples for pollen analysis from the bog profile, from the surface down to 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 ...

    • 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 ...

    • 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 ...

    • 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 ...

    • 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. ...

    • Skoggrænsens og sneliniens større høide tidligere i det sydlige Norge 

      Rekstad, Johan (NGU (36), Journal article, 1903)
      Forkortet: In the mountainous regions of the Southern Norway, logs and roots of the red fir (pinus sylvestris) are found in the bogs much higher, than this tree grown here, at the present day. This is mentioned by many ...