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
Crown Colony of Malta French rule and asked Britain for help. Eventually, the French capitulated in 1800 and Malta voluntarily became a British protectorate. Britain was then supposed to evacuate the island according to the terms of the Treaty of Amiens of 1802, but failed to keep this obligation – one of several mutual cases of non-adherence to the treaty, which eventually led to its collapse and the resumption of war between Britain and France a year later. Malta became a Crown Colony on 23 July 1813, when Sir Thomas Maitland was appointed as Governor of Malta. That year, Malta was granted the Bathurst