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  • Six tsunami scenarios were simulated in a numerical model, namely with tripartite tsunami wave trains approaching from west, south-west and south, and with 2 different intensities (moderate and extreme). Both, in the moderate and extreme scenarios
  • . Both, simulation results and field evidence support the Olympia Tsunami Hypothesis, suggesting that ancient Olympia was destroyed and buried by repeated tsunami-related flooding of the coast along the Kyparissiakos Gulf. The regional tsunami risk has
  • The AA. summarise and review individual observations of both : earthquake and tsunami that occurred along the Makran Subduction Zone on 27 November, 1945. Published scientific reports, newspaper articles as well as eyewitness accounts are used
  • . High-energy dislocated boulders showed no movement during the monitoring period. Thus, it is assumed that they were been transported inland by extreme events, which were stronger than the average coastal dynamics between 2009 and 2011. Both
  • the underlying Pleistocene relief. Geochronology is based on radiocarbon ages and on pollen and macro-remains of encountered Holocene peat layers. XRF-data obtained by both stationary and handheld scanning techniques was used to trace interferences of different