1905 Calabria earthquake
Striking southern Italy on 8 September, the 1905 Calabria earthquake had a moment magnitude of 7.2 and a maximum Mercalli intensity of XI (Extreme).The first major earthquake of the 20th century, it severely damaged parts of Lipari, Messina Province and a large area between Cosenza and Nicotera and killed between 557 and 2,500 people.The initial result of the rollback was the formation of the Tyrrhenian Sea back-arc basin starting in the Miocene, continuing in to the Pleistocene.[12] It has also been suggested that the earthquake was a result of a normal fault rupture within the slab of African plate oceanic crust subducting beneath Calabria, at a depth of 35–55 km.[10] The submarine telegraph cable connecting the Aeolian Islands to Milazzo on Sicily was broken at a depth of 1180 m, presumably by a turbidity current caused by slope failure triggered by the earthquake.[15] Evidence of ground fissures and liquefaction was widespread and many streams and springs were changed in both flow rate and temperature, immediately after the earthquake.He noted that structures built on limestone, molasse, breccia and schist suffered the greatest damage, while those constructed on granite fared much better.In October 1906 the Prefect of Cantanzaro reported that many families remained homeless, while those in the shacks were affected by their poor quality, with both wind and rain being able to penetrate these structures.