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  • 1. Jakobsson, M.
    et al.
    Anderson, J. B.
    Corrugation ridges in the Pine Island Bay glacier trough, West Antarctica2016In: Geological Society Memoir, ISSN 0435-4052, E-ISSN 2041-4722, Vol. 46, no 1, p. 265-266Article in journal (Refereed)
    Abstract [en]

    Glacial landforms with dimensions smaller than the imaging capability of the first-generation multibeam sonars will become a more frequent topic as high-resolution seafloor mapping technology advances. In Pine Island Bay (PIB) glacial trough, West Antarctica, small regular ridges of only a few metres from trough to crest were mapped in water depths of about 700 m. The small size of these ridges is at the limit of what modern deep-water multibeam sonars are capable of mapping. The ridges are interpreted to have been formed at the trailing edge of mega-icebergs moving up and down in response to tides while ploughing the seafloor (Jakobsson et al. 2011). The mega-icebergs in PIB were produced by ice shelf break-up and associated grounding-zone retreat.

  • 2. Jakobsson, M.
    et al.
    Gyllencreutz, R.
    Mayer, L. A.
    Dowdeswell, J. A.
    Canals, M.
    Todd, B. J.
    Dowdeswell, E. K.
    Hogan, K. A.
    Larter, R. D.
    Mapping submarine glacial landforms using acoustic methods2016In: Geological Society Memoir, ISSN 0435-4052, E-ISSN 2041-4722, Vol. 46, no 1, p. 17-40Article in journal (Refereed)
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