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) months, starting from around mid-April with temperatures during the day and at night, ending in November with temperatures during the day and at night, although also in the remaining 4 months temperatures sometimes reach . Amongst all capitals in the continent of Europe, Valletta – the capital of Malta has the warmest winters, with average temperatures of around during the day and at night in the period January–February. In March and December average temperatures is around during the day and at night. Large fluctuations in temperature are rare. Also, Malta is one of the few places in Europe which are