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On the morning of 21 July 365 AD, a large earthquake caused a tsunami more than 100 feet (30 m) high, devastating Alexandria and the eastern and southern shores of the Mediterranean, killing many thousands, and hurling ships nearly two miles inland.
The fate of the city, which remained permanently submerged, was often commented upon by ancient writers Underwater geoarchaeological excavations on the shallow shelf (∼10 m depth) at Caesarea, Israel, have documented a tsunami that struck the ancient harbor at Caesarea. The tsunami was probably triggered by an earthquake that destroyed Antioch, and was generated somewhere on the Cyprian Arc fault system.
Talmudic sources record a tsunami that struck on 13 December A. Many cities were flooded by the sea, with the cities of Roman Asia reporting the worst tsunami damage.
Because of seismic and volcanic activity associated with tectonic plate boundaries along the Pacific Ring of Fire, tsunamis occur most frequently in the Pacific Ocean, but are a worldwide natural phenomenon.
They are possible wherever large bodies of water are found, including inland lakes, where they can be caused by landslides and glacier calving.