Geology of Malta elephant fossils), as well as island gigantism (fossils of Leithia melitensis). 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
Malta (island) under Napoleon occupied Malta and ruled from 1798-1800. Napoleon's stay lasted from 12–18 June when he resided at Palazzo Parisio in Valletta. The French remained until the Maltese rebelled against their rule. In 1800, the British took control over Malta and the island initially became a British protectorate, and a colony a couple of years later. The British ruled for about 150 years and Malta became independent in 1964. Ten years later the State of Malta became the Republic of Malta. Malta joined the European Union in 2004 and adopted the Euro four years later. Malta is the largest island