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
Cornwallis Island (Nunavut) the north end of McDougall Sound, which separates Cornwallis Island from nearby Bathurst Island. Cape Airy is located at the island's southwestern extremity. Also on the southwestern coast, Griffith Island lies directly across from the island's populated hamlet Resolute (Qausuittuq), separated by the wide Resolute Passage. The airport at Resolute acts as a communications hub for the central Arctic islands of Nunavut. This is Canada's second most northerly community. The first European to visit Cornwallis Island was Sir William Edward Parry in 1819, and is named for British Royal Navy admiral Sir William Cornwallis. Cornwallis Island is also home to