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
Malta and architectural and historical monuments, including three UNESCO World Heritage Sites: Hypogeum of Ħal-Saflieni, Valletta, and seven megalithic temples which are some of the oldest free-standing structures in the world. The origin of the name "Malta" is uncertain, and the modern-day variation is derived from the Maltese language. The most common etymology is that the word "Malta" is derived from the Greek word , "meli", "honey". The ancient Greeks called the island ("Melitē") meaning "honey-sweet", possibly for Malta's unique production of honey; an endemic subspecies of bee lives on the island. The Romans called the island "Melita", which can be