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,
Harkers Island, North Carolina mostly white sand on rolling dunes. Harkers Island is protected from the Atlantic Ocean by the barrier islands of the Shackleford Banks to the south and the Core Banks to the east. The body of water directly south of the island is Back Sound. To the east is Core Sound, to the north is The Straits, and to the northwest is the mouth of the North River. The Straits are shallow but navigable by those with local experience. There are two small bays on the north side of the island, Westmouth Bay and Eastmouth Bay. North of Eastmouth Bay is