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,
Palazzo Malta the French forces under Napoleon Bonaparte was seen over the horizon of the island of Malta, Malta had been the base of the Order of St. John of Jerusalem, also called the Order of Malta. The Order had been given the island by Charles V, Holy Roman Emperor in 1530. Napoleon left the island with a sizeable garrison and a handpicked administration. Following a Maltese uprising, the British Lord Nelson was asked and took over Malta on 5 September 1800. Malta was made a British colony on 30 March 1814 by the Treaty of Paris. Thus, the Order of Malta