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,
Sovereign Military Order of Malta island of Malta, the Embassy of the Order to Holy See and the Embassy of the Order to Italy have all been granted extraterritoriality by Italy and Malta. Unlike the Holy See, however, which is sovereign over Vatican City and thus has clear territorial separation of its sovereign area and that of Italy, SMOM has had no territory since the loss of the island of Malta in 1798, other than only those current properties with extraterritoriality listed above. Italy recognizes, in addition to extraterritoriality, the exercise by SMOM of all the prerogatives of sovereignty in its headquarters. Therefore, Italian sovereignty