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) the world highlighting the emerging strength of Malta as a jurisdiction for banking and finance and insurance. Traffic in Malta drives on the left. Car ownership in Malta is exceedingly high, given the very small size of the island. The main roads of Malta from the southernmost point to the northernmost point are these: Triq Birżebbuġa in Birżebbuġa, Għar Dalam Road and Tal-Barrani Road in Żejtun, Santa Luċija Avenue in Paola, Aldo Moro Street (Trunk Road), 13 December Street and Ħamrun-Marsa Bypass in Marsa, Regional Road in Santa Venera/Msida/Gżira/San Ġwann, St Andrew's Road in Swieqi/Pembroke, Malta, Coast Road in Baħar