Blar i Norwegian Geotechnical Institute (NGI) Digital Archive på forfatter "Forsberg, Carl Fredrik"

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    • A climatic trigger for the giant Troll pockmark field in the northern North Sea 

      Mazzini, Adriano; Svensen, Henrik; Forsberg, Carl Fredrik; Linge, Henriette; Lauritzen, Stein-Erik; Haflidason, Haflidi; Hammer, Øyvind; Planke, Sverre; Tjelta, Tor-Inge (Journal article; Peer reviewed, 2017)
      Pockmarks are seafloor craters usually formed during methane release on continental margins. However, the mechanisms behind their formation and dynamics remain elusive. Here we report detailed investigations on one of the ...

    • Fluid flow and pore pressure development throughout the evolution of a trough mouth fan, western Barents Sea 

      Llopart, J.; Urgeles, R.; Forsberg, Carl Fredrik; Camerlenghi, A.; Vanneste, Maarten; Rebesco, M.; Lucchi, Renata Giulia; Rüther, Denise Christina; Lantzsch, H. (Peer reviewed; Journal article, 2018)
      Using a combination of geophysical and geotechnical data from Storfjorden Trough Mouth Fan off southern Svalbard, we investigate the hydrogeology of the continental margin and how this is affected by Quaternary glacial ...

    • Landslide Material Control on Tsunami Genesis ‐ The Storegga Slide and Tsunami (8100 y BP) 

      Kim, Jihwan; Løvholt, Finn; Issler, Dieter; Forsberg, Carl Fredrik (Peer reviewed; Journal article, 2019)
      Tsunami generation from sub‐aqueous landslides is controlled by landslide kinematics, which in turn is governed by the material properties of the slide mass. Yet, the effect of the material properties on tsunami‐genesis ...

    • NE Atlantic continental slope stability from a numerical modeling perspective 

      Bellwald, Benjamin; Urlaub, Morelia; Hjelstuen, Berit Oline Blihovde; Sejrup, Hans Petter; Sørensen, Mathilde B.; Forsberg, Carl Fredrik; Vanneste, Maarten (Peer reviewed; Journal article, 2018)
      Trough mouth fans are environments characterized by high sediment supply during glacial stages and the occurrence of large-scale instabilities. The geological record indicates that several of these environments have failed ...