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,
North Manitou Island North Manitou Island North Manitou Island is located in Lake Michigan, approximately west-northwest of Leland, Michigan. It is nearly eight miles long and over four miles (6 km) wide, with of shoreline. It has a land area of 57.876 km (22.346 sq mi) and has no population. The smaller South Manitou Island lies to its southwest. North Manitou Island is shaped like an upside-down teardrop, with the now-forested body of the 'drop' surrounding Lake Manitou, and the tail of the drop narrowing into sandy, exposed Dimmick's Point on the island's southeastern extremity. The ferry dock and ranger station are on