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
North Stradbroke Island Advisory Board, constituted by two members from each of the island's townships and an executive chairperson. However, no Quandamooka people, who had their native title claim recognised in July 2011, after a 16-year proceeding, are members of the board of this community fund. As at October 2017, there is no reference to the community fund on the Sibelco website. North Stradbroke Island North Stradbroke Island (Jandai: Minjerribah), colloquially "Straddie" or "North Straddie", is an island that lies within Moreton Bay in the Australian state of Queensland, southeast of the capital Brisbane. Before 1896 the island was part of the Stradbroke