Blar i Artikler på emneord "LANDHEVNING"

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    • Beskrivelse til kartbladet Dønna 

      Rekstad, Johan (NGU (37), Journal article, 1904)
      Forkortet: This region is situated in the Northern part of the district of Helgeland between 66\u00B0 and 66\u00B0 20' N. A geological map in black is given on pages 4 and 5. The igneous rocks here are granites, gabbro and ...

    • Norges hevning etter istiden 

      Rekstad, J. (NGU (96), Journal article, 1922)
      The present paper is in substance an explanatory text accompanying a map of the post-glacial changes of level in the Scandinavian peninsula. At the end of the Glacial Period the Scandinavian peninsula was more deeply ...

    • 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 ...

    • 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 ...

    • Strandliniens beliggenhed under stenalderen i det sydøstlige Norge 

      Brøgger, Wilhelm C. (NGU (41), Journal article, 1905)
      Forkortet: Die Lage der Strandlinie w\u00E4hrend der verschieden Abschnitte der postglacialen Hebung. Zur L\u00F6sung dieser Aufgabe wurde eine Revision der fr\u00FCheren Untersuch- ungen \u00FCber die gleichzeitigen ...

    • Strandlinjer, moræner og skjælforekomster i den sydlige del av Troms fylke 

      Grønlie, Ole T. (NGU (94), Journal article, 1922)
      Within the Ofoten territory there are 5 good shore-lines as elsewhere in Northern Norway and besides these there is a 6th line farther to the north only observed near the heads of the fjords. These 6 lines have been measured ...