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New Hebrides, officially the New Hebrides Condominium (French: Condominium des Nouvelles-Hébrides) and named after the Hebrides in Scotland, was the colonial name for the island group in the South Pacific Ocean that is now Vanuatu.
The New Hebrides Trench (perhaps better termed the South New Hebrides Trench) [1] [2] is an oceanic trench which is over 7.1 km (4.4 mi) deep in the Southern Pacific Ocean. [3] It lies to the northeast of New Caledonia and the Loyalty Islands , to the southwest of Vanuatu (formerly known as the New Hebrides ), east of Australia, and south of ...
Malakula, also spelled Malekula, is the second-largest island in the nation of Vanuatu, formerly the New Hebrides, in Melanesia, a region of the Pacific Ocean. Location [ edit ]
An expandable bathymetric and topographic map of New Caledonia and Vanuatu, formerly the New Hebrides.Click to enlarge. New Caledonia is made up of a main island, the Grande Terre, and several smaller islands, the Belep archipelago to the north of the Grande Terre, the Loyalty Islands to the east of the Grande Terre, the Isle of Pines to the south of the Grande Terre, the Chesterfield Islands ...
The zone includes most of the islands of Vanuatu, the Santa Cruz islands of the southern Solomon Islands, [4] and the Loyalty Islands.A number of ocean floor features are related to the zone, in particular the New Hebrides Trench (South New Hebridies Trench) [5] and the North New Hebrides Trench (Torres Trench) which is separated from the southern trench by the d'Entrecasteaux Ridge and the ...
Vanuatu (formerly called the New Hebrides) is a nation and group of islands in the South Pacific Ocean. It is composed of over 80 islands with 2,528 kilometres (1,571 mi) of coastline and a total surface area of 12,189 square kilometres (4,706 sq mi). It's a small country with a total size of 12,189 km 2 (4,706 sq mi).
The Hebrides have a diverse geology, ranging in age from Precambrian strata that are amongst the oldest rocks in Europe, to Paleogene igneous intrusions. [2] [3] [Note 1] Raised shore platforms in the Hebrides have been identified as strandflats, possibly formed during the Pliocene period and later modified by the Quaternary glaciations.
At the start of the war Espiritu Santo was one of a string of roughly 80 islands under the rule of a joint British and French New Hebrides colony. The administration was the Anglo-French Condominium of the New Hebrides. U.S. troops first set up a base in May 1942 on the nearby island of Efate, as a defence against the expanding Imperial Japan. [8]