• Deglaciation of the continental shelf off southern Troms, North Norway. 

      Vorren, Tore O.; Thomsen, Elsebeth; Hald, Morten; Edvardsen, Magne (NGU (380), Journal article, 1983)
      Based on lithostratigraphical and seismic studies, four (possibly five) glacial events are recognized in Andfjorden. The two oldest, the I- and G-events are represented by basal tills. The continental ice sheet probably ...
    • Development of minor late-glacial ice domes east of Oppdal, Central Norway 

      Follestad, Bjørn A. (NGU Bulletin (441), Journal article, 2003)
      Glacial striations and ice-marginal forms such as lateral moraines and meltwater channels show that a major north-westerly-directed ice flow invaded the Oppdal area prior to the Younger Dryas (YD) Chronozone. Through the ...
    • Dybderne i nogle indsjøer i Jotunfjeldene og Thelemarken 

      Helland, Amund (NGU (14), Journal article, 1894)
      Many of our lakes are very deep; some of them are deeper than the bottom of the sea nearest to them. The depths are given in metres
    • Kartlegging av glasiale landformer på Søre Sunnmøre 

      Christoffersen, Marianne; Fredin, Ola; Larsen, Eiliv; Lyså, Astrid; Nordahl, Bo (NGU-Rapport (2021.002), Report, 2021)
      I 2020 har Norges geologiske undersøkelse (NGU) i samarbeid med Artsdatabanken videreført arbeidet med utvikling av metoder og prosedyrer for kartlegging av glasiale landformer som ble påbegynt i 2019. Kartleggingen har ...
    • Kartlegging av glasiale landformer: pilotprosjekt 2019 

      Christoffersen, Marianne; Fredin, Ola; Larsen, Eiliv; Lyså, Astrid; Nordahl, Bo (NGU-Rapport (2020.001), Report, 2020)
      I områder av Agder og Trøndelag har Norges geologiske undersøkelse (NGU) i samarbeid med Artsdatabanken startet utvikling av metoder og prosedyrer for mest mulig operatøruavhengig kartlegging av glasiale landformer. Områdene ...
    • 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 ...
    • Lokalglaciasjon på Sunnmøre. (On the mountain glaciation of Sunnmøre, West-Norway.) 

      Reite, Arne J. (NGU (247), Journal article, 1967)
      Terminal moraines deposited by cirque glaciers are described from Sunnmøre, West Norway. Radiocarbon dating indicates that the fjord districts were free from inland ice in Allerød time. The mountain glaciation most likely ...
    • Moraines in the Hemnefjord area, Western Norway. 

      Lasca, N.P. (NGU (266), Journal article, 1970)
      Four radiocarbon dates are used to date moraines in the inner Hemnefjord area. The radiometric ages of moraines range from approximately 10,720 to 11,310 years B.P. and probably correlate with the Ra moraines in Southern ...
    • Nogle bidrag til forstaaelsen af, hvorledes Norges dale og fjelde er blevne til 

      Reusch, Hans (NGU (32), Journal article, 1901)
      Forkortet: Up to the present, the relief of Norway has not been understood sufficiently to allow of a satisfactory explanation being given of even the most salient features, such as the contrast between plateau and valley, ...
    • The surface of the inland ice in the Atndalen valley, South-central Norway. 

      Follestad, Bjørn A. (NGU Bulletin (438), Journal article, 2001)
      On the basis of different field observations, several authors have discussed the form of the inland ice in southern Norway. In this work, lateral features indicating the upper limit of zones of meltwater drainage marked ...