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Run-up height, inundation distance and spatial extension of the erosion and deposition pattern are the key elements to determine the impact of a tsunami. Calibration or recalibration of each date was based on OxCal v4. Naruse, H. The stratigraphic position is close to the one observed at Fethiye and the dates obtained in the tsunamites are very close to those obtained in the Malia tsunamites, even if the margins of error remain too large.
