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
Pembroke, Malta Pembroke, Malta Pembroke is a town in the Northern Region of Malta, and it is considered to be the country's newest town. To the east is Paceville, the nightlife district of Malta. The coastal town and tourist hub of St. Julian's lies to the southeast, and the residential area of Swieqi lies to the south. The hilltop village of Madliena is to its west, and Baħar iċ-Ċagħaq lies to the northwest. Pembroke covers an area of 2.3 km². The area hugs a coastal zone with a rocky beach. The highest point lies at 64 meters (210 feet) above sea level