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  • 1. Long, A J
    et al.
    Smith, D E
    Mörner, Nils-Axel
    Dawson, S
    Final Report of the INQUA Shorelines Subcommission on Western Europe2005In: Journal of Coastal Research, ISSN 0749-0208, 43-51 p.Article in journal (Refereed)
    Abstract [en]

    We provide a short report on the final year of the INQUA Shorelines Subcommission on Western Europe (2002-3). This includes a review of activities under four themes: sea-level changes in the next century; sea-level changes along a north-south transect from the uplifting coasts of Fennoseandanvia to the subsiding coasts of the North Sea and the Baltic, and the meta stable areas such as Portugal and France; comparisons between modeled and empirical observations of relative sea-level (RSL) change, and palaeo-tsunami and storm records. We conclude by providing a report on the final 2002 Annual Meeting including its field meeting at Greifswald and Mecklenburg-West Pomerania and provide a list of some recent publications by members of the INQUA Shorelines Subcommission.

  • 2. Mörner, Nils-Axel
    et al.
    Laborel, Jacques
    Dawson, Sue
    Submarine "Sandstorms" and Tsunami Events in the Indian Ocean2008In: Journal of Coastal Research, ISSN 0749-0208, Vol. 24, no 6, 1608-1611 p.Article in journal (Refereed)
    Abstract [en]

    The December 26, 2004, disastrous tsunami event in the Indian Ocean may have come as a shock and even a surprise to the communities outside geosciences. However, tsunami events are a natural part of the geosystems in regions of submarine earthquakes, and they will continue to hit the region even in the future. Here we present evidence of former tsunami events both on Sri Lanka and on the Maldives. Submarine "sandstorms" driven by tsunami waves brought littoral deposits down into eaves 21 to 38 m below sea level. Radiocarbon dates allow the comparison with related tsunami signals in fens and lagoons, and historical documentation. The terrible December 26 event has raised a general awareness of tsunami events. It has also generated the installation of necessary warning systems. We are in urgent need, however, of a long-term tsunami chronology for a realistic tsunami hazards assessment.

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