• Diatom stratigraphy related to Late Weichselian sea-level changes in Sunnmøre, Western Norway. 

      Lie, Sven Erik; Mangerud, Jan; Stabell, Bjørg (NGU (380), Journal article, 1983)
      In sediment cores from four small basins from 44 to 26 m above sea-level, the boundaries between marine, brackish and lacustrine sediments are precisely identified through their distinct diatom stratigraphy. In all basins ...
    • En rekonstruksjon av isbevegelser under siste istid i Samnanger og Kvam, Hordaland, Vest-Norge. 

      Hamborg, Martin; Mangerud, Jan (NGU (369), Journal article, 1981)
      The reconstructions are based mainly on analysis of glacial striae. The oldest striae indicate that the glacier flow, was influenced by the deep Hardangerfjord, even during the Weichselian maximum. Younger striae of assumed ...
    • Glasialgeologi og vegetasjonsinnvandring i Indre Nordhordland, Vest-Norge. 

      Aa, Asbjørn Rune; Mangerud, Jan (NGU (369), Journal article, 1981)
      In the area between Hardangerfjorden and Sognefjorden an oldest regional ice movement towards the west has been reconstructed. Younger regional ice movements were towards south-west in the southern parts. Therefore, an ...
    • Isavsmelting i og omkring midtre Gudbrandsdalen. 

      Mangerud, Jan (NGU (223), Journal article, 1963)
      Observed glacial striae showing direction of ice-movement during the last active stage of the inland-ice are shown in fig. 1. Supposed major directions of ice movement are also shown in fig. 3. In the mountain parts are ...
    • 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 ...