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,
Malta (island) are 54 local councils and 13 administrative committees in Malta. The island is also divided into five districts, but these serve primarily for statistical purposes: Malta (island) Malta is the largest of the three major islands that constitute the Maltese archipelago. It is sometimes referred to as Valletta for statistical purposes to distinguish the main island from the entire country. Malta is in the middle of the Mediterranean Sea directly south of Italy and north of Libya. The island is long and wide, with a total area of . The capital is Valletta, largest locality is Birkirkara. The island is