The AD 365 Crete Earthquake/Tsunami Submarine Impact on the Mediterranean Region

The Calabrian and Hellenic subduction systems accommodate the African Eurasian plate convergence in the Mediterranean Sea and are the site of large earthquakes in the forearc region facing the northern African coasts. Some of the historical earthquakes were associated with the generation of tsunami waves affecting the entire Mediterranean basin. We investigated the submarine effects of the AD 365 Crete earthquake on the sedimentary records through the integrated analysis of geophysical data, turbidite deposits, and tsunami modelling. Seismic reflection images show that some turbidite beds are thick and marked by acoustic transparent layers at their top. Radiometric dating of the most recent of such mega-beds, the Homogenite/Augias turbidite (HAT), provide evidence for synchronous basin-wide sedimentation during a catastrophic event which has occurred in the time window of AD 364–415, consistent with the AD 365 Mw = 8.3–8.5 Crete earthquake/tsunamis. The HAT (up to 25 m thick) contains components from different sources, implying remobilization of material from areas very far from the epicentre. Utilizing the expanded stratigraphy of the HAT and the heterogeneity of the sediment sources of the Mediterranean margins, we reconstructed the relative contribution of the Italian, Maltan and African margins to the turbidite deposition. Our sedimentological reconstructions combined with tsunami modelling suggest that the tsunami following the Crete earthquake produced giant turbidity currents along a front over 2000 km long, from northern Africa to Italy. Our cores suggests that during the last 15,000 years, only two similar turbidites have been deposited in the deep basins, pointing to a large recurrence time of such extreme sedimentary events.