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Ogasawara Islands |
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Ogasawara IslandsThe Ogasawara Islands (小笠原諸島) are an archipelago of over 30 subtropical islands some 1000 km directly south of central Tokyo, Japan. Administratively, they are a part of Tokyo. The islands are also known as the Bonin Islands, and the southernmost (uninhabited) group is known as the Volcano Islands.The only inhabited islands are Chichi-jima (父島, lit. "Father Island") and Haha-jima (母島, "Mother Island"). Access to these islands is possible only via a single weekly overnight ferry from Tokyo, although there are plans to open an airport. Tourists are attracted to the islands by scuba diving and whale watching. The uninhabited Iō-jima (硫黄島, "Sulphur Island"), better known in English as Iwo Jima, is a part of the Volcano Islands. Access to the island requires special permission. GeologyThe Ogaswara islands are a volcanic island arc. They lie at the junction of the Pacific Plate and the Philippine Plate. The Pacific Plate is subducting under the Philippine Plate, which creates an oceanic trench to the east of the islands. The islands were formed by volcanic activity caused by the subducting plate, and are composed mostly of an andesitic volcanic rock called Boninite, which is rich in magnesium oxide, chromium, and silicon dioxide. The basal rocks of the islands range from 65 to 1.8 million years old. The volcano on Iō-jima, Mount Suribachi, is believed extinct. Most of the islands have steep shorelines, often with sea cliffs ranging from 50 to 100 meters in height. Several of the islands are fringed with coral reefs. HistoryThe first recorded settlement of the islands was an American colony founded in 1830, which persisted until the Second World War. Japan has ruled the islands since 1875. Ogasawara subtropical moist forestsThe Ogasawara Islands form a distinct subtropical moist broadleaf forest ecoregion, with a high degree of biodiversity and endemism. The islands are home to about 500 plant species, of which 43% are endemic. The forests are of three main types:
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