Geography of New Caledonia point is Mont Panié at elevation. The total area of New Caledonia is , of those being land. A territorial dispute exists with regard to the uninhabited Matthew and Hunter Islands, which are claimed by both France (as part of New Caledonia) and Vanuatu. The New Caledonian archipelago is a microcontinental island chain which originated as a fragment of Zealandia, a nearly submerged continent or microcontinent which was part of the southern supercontinent of Gondwana during the time of the dinosaurs. The Grande Terre group of New Caledonia, with Mont Panié at as its highest point, is the most elevated
Biodiversity of New Caledonia the view of the island as a surviving fragment of the Cretaceous period is obsolete. Islands from that time are partly or fully submerged. Most modern New Caledonian terranes formed via accretion of oceanic island arcs and seamounts. The biota evolved as metapopulations on islands that changed constantly until they merged into the archipelago. This hypothesis that the islands and their biota emerged some 30 MYA during the Oligocene better explains the organisms that occur in New Caledonian biota. In the Carboniferous and Permian, New Zealand and New Caledonia were on the periphery of Gondwana, which included Africa, South America,