UDK 550.344.4(261.26)"633" Documenta Praehistorica XXXV (2008) The catastrophic final flooding of Doggerland by the Storegga Slide tsunami Bernhard Weninger1, Rick Schulting2, Marcel Bradtmöller3, Lee Clare1, Mark Collard4, Kevan Edinborough4, Johanna Hilpert1, Olaf Jöris5, Marcel Niekus6, Eelco J. Rohling7, Bernd Wagner8 1 Universität zu Köln, Institut für Ur- und Frühgeschichte, Radiocarbon Laboratory, Köln, D,
[email protected]< 2 School of Archaeology, University of Oxford, Oxford, UK< 3 Neanderthal Museum, Mettmann, D< 4 Laboratory of Human Evolutionary Studies, Dpt. of Archaeology, Simon Fraser University, Burnaby, CDN< 5 Römisch Germanisches Zentralmuseum Mainz, D< 6 Groningen Institute of Archaeology, Groningen, NL< 7 School of Ocean and Earth Science, National Oceanography Centre, Southampton, UK< 8 Universität zu Köln, Institut für Geologie und Mineralogie, Köln, D ABSTRACT Ð Around 8200 calBP, large parts of the now submerged North Sea continental shelf (‘Dog- gerland’) were catastrophically flooded by the Storegga Slide tsunami, one of the largest tsunamis known for the Holocene, which was generated on the Norwegian coastal margin by a submarine landslide. In the present paper, we derive a precise calendric date for the Storegga Slide tsunami, use this date for reconstruction of contemporary coastlines in the North Sea in relation to rapidly rising sea-levels, and discuss the potential effects of the tsunami on the contemporaneous Mesolithic popula- tion. One main result of this study is an unexpectedly high tsunami impact assigned to the western regions of Jutland. IZVLE∞EK – Okoli 8200 calBP je velik del danes potopljenega severnomorskega kontinentalnega pasu (Doggerland) v katastrofalni poplavi prekril cunami. To je eden najvejih holocenskih cunamijev, ki ga je povzroil podmorski plaz na norve¸ki obali (Storegga Slide).