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,
Three villages of Malta Three villages of Malta The Three Villages of Malta are Attard, Balzan, and Lija, which are located approximately at the centre of the Mediterranean island of Malta. The Three Villages are known as such because of their close proximity to one another. In some cases one side of the street is part of one village while the opposite side of the same street is part of another village. The three villages are also very similar in size, layout and age. During the Order of St. John the three villages were sought after for country residences and hunting lodges, of which