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 Malta Malta (, ; ), officially known as the Republic of Malta (), is a Southern European island country consisting of an archipelago in the Mediterranean Sea. It lies south of Italy, east of Tunisia, and north of Libya. With a population of about 475,000 over an area of , Malta is the world's tenth smallest and fifth most densely-populated country. Its capital is Valletta, which is the smallest national capital in the European Union by area at 0.8 km. The official languages are Maltese and English, with Maltese officially recognised as the national language and the only Semitic language