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) there are minorities, the largest of which are British, many of whom have retired to Malta. According to the government's estimate of 2013, the population of Malta stood at 409,259 people which is about 91.6% of the country's total population. The largest city is Birkirkara with a population of 22,319. The capital Valletta has a relatively small population of 6675 people. The main language spoken on Malta is the Maltese language, a Semitic language descended from the now defunct Siculo-Arabic dialect of southern Italy. The language has substantial borrowing from Sicilian, Italian, a little French, and more recently and increasingly,