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) now travel abroad on holiday. In recent years, Malta has advertised itself as a medical tourism destination, and a number of health tourism providers are developing the industry. However, no Maltese hospital has undergone independent international healthcare accreditation. Malta is popular with British medical tourists, pointing Maltese hospitals towards seeking UK-sourced accreditation, such as with the Trent Accreditation Scheme. Dual accreditation with the American-oriented Joint Commission is necessary if hospitals in Malta wish to compete with the Far East and Latin America for medical tourists from the United States. Native Maltese people make up the majority of the island. However,