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) fields. The highest point in Malta is Ta' Dmejrek, at , near Dingli. Although there are some small rivers at times of high rainfall, there are no permanent rivers or lakes on Malta. However, some watercourses have fresh water running all year round, such as those at Ras ir-Raħeb near Baħrija and at l-Imtaħleb. Phytogeographically, Malta belongs to the Liguro-Tyrrhenian province of the Mediterranean Region within the Boreal Kingdom. According to the WWF, the territory of Malta belongs to the ecoregion of "Mediterranean Forests, Woodlands and Scrub". Some minor islands off the main island of Malta include: Malta has a