1783 Calabrian earthquakes

[2] This earthquake, with an estimated magnitude of 7.0, affected a large area including most of the southern Italian peninsula and shook the whole island of Sicily.

Near the epicenter the ground shaking was so intense that people were knocked off their feet and heavy stones were found to be dislodged and upturned.

[1] Large landslides caused major destruction at Terranova and Molochio but even well-constructed buildings not thus affected were almost completely destroyed, such as in Oppido Mamertina and Casalnuovo.

[1] The earthquake is thought to have involved rupturing of the Galatro, Cittanova and Sant'Eufemia faults, which form the southeastern boundary to the Gioia Basin.

Most of the damage and casualties appear to have been caused by a tsunami that was set off by a major collapse of Monte Pací into the sea near Scilla shortly after the earthquake.

[1] The final event of the sequence was of similar magnitude to the first and had an epicenter about 20 km east of the fourth, near Girifalco and Borgia in the Catanzaro Basin.

Main faults of the Siculo-Calabrian rift zone
Contemporary print of the February 5 earthquake