Geology of Malta Geology of Malta 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. The Maltese archipelago is situated on the mainly shallow water continental platform between Sicily and North Africa that lies beneath the Sicily Channel, separating the Ionian Basin from the western Mediterranean Basin. The islands lie around 200 km to the south of the subduction boundary between the African Plate and the Eurasian Plate. The platform is crossed by a rift zone formed of three grabens: the Pantelleria graben,
Crown Colony of Malta Crown Colony of Malta The Crown Colony of the Island of Malta and its Dependencies (commonly known as the Crown Colony of Malta) was a British colony in the present-day Republic of Malta. It was established when the Malta Protectorate was transformed into a British Crown colony in 1813, and this was confirmed by the Treaty of Paris in 1814. From 1530 to 1798, Malta had been ruled by the Order of Saint John. The Order was ousted during the War of the Second Coalition and Malta was occupied by Napoleon. The Maltese rebelled after a couple of months of