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Matthew and Hunter Islands
The Matthew and Hunter Islands are a group of two small and uninhabited high islands in the South Pacific, located east of New Caledonia and south-east of Vanuatu archipelago. Hunter Island and Matthew Island, apart, are claimed by Vanuatu as part of Tafea Province, and considered by the people of Aneityum part of their custom ownership, and as of 2007 were claimed by France as part of New Caledonia.〔(SMALL ISLANDS VOICE )〕
Small, arid, without fresh water and not easily accessible, the islands had no interest for Britain or France during their colonization of the Pacific in the course of the 18th and 19th centuries. France officially annexed both islands in 1929. In 1965, the United Kingdom also claimed the two islands, as part of the New Hebrides. France conducted a symbolic occupation in 1975. In 1980, on its independence, Vanuatu claimed sovereignty, but made no occupation of the islands. In 1979, Météo-France set up an automatic weather station on one of the islands, and the French Navy regularly visits both of them.
==Matthew Island==
Matthew Island ((フランス語:île Matthew)) is in area, with a high stratovolcano located at . The volcanic island is composed of two andesitic-to-dactic volcanic cones, East Matthew and West Matthew, separated by a rocky 200-metre-wide isthmus. The island was discovered by Captain Thomas Gilbert of the Royal Navy on board the ''Charlotte'' on 27 May 1788, who named it after the owner of his ship. At the time of the discovery, only East Matthew existed and it was described as having only one peak prior to the Second World War.
East Matthew is the older part of the island, formed from basalt with a half-destroyed, 142-m-high composite volcanic cone that is thought to be composed of three lava flows. There is still some volcanic activity on the island with sulphuric fumaroles rising from craters in the south-east. West Matthew formed in the late 1940s and may have had eruptions as recent as 1976. It is a roughly circular, 177-m-high cone with a serrated peak and is composed almost entirely of lava flows and slag. It contains a crater that is breached to the northwest. A lava flow from West Matthew makes up the northwest coast of the island.
抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』
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