Seismic risk in Malta is considered to be low with little historic damage noted and no known victims. The archipelago is however in a potentially significant seismic zone and the risk to the population is probably undervalued.
German copper engraving dating from 1696 on the Sicilian earthquake
St. Paul's Cathedral, Mdina, rebuilt after the 1693 earthquake, damaged by the 1743 earthquake
Għajn Ħadid Tower, which collapsed in the 1856 earthquake
Fort Chambray in Gozo
The Geology of Malta consists of a sequence of sedimentary rocks of late Oligocene to late Miocene age cut through by a set of extensional faults of Pliocene age.
Cliffs of Upper Globogerina Limestone Formation at Il-Ħofra l-Kbira near Marsaxlokk
Dingli cliffs showing stratification in the Lower Coralline Limestone
Hardground at the top of the Lower Coralline Limestone Formation with limestone clasts and fossils of the echinoid Scutella subrotunda and bivalves
Limestone wall showing honeycomb weathering