Izu–Bonin–Mariana Arc
The Izu–Bonin–Mariana (IBM) arc system is a tectonic plate convergent boundary. The IBM arc system extends over 2800 km south from Tokyo, Japan, to beyond Guam, and includes the Izu Islands, the Bonin Islands, and the Mariana Islands; much more of the IBM arc system is submerged below sealevel. The IBM arc system lies along the eastern margin of the Philippine Sea Plate in the Western Pacific Ocean. It is the site of the deepest gash in Earth's solid surface, the Challenger Deep in the Mariana Trench.
1855 Edo earthquake
D'Entrecasteaux Ridge
East Diamante
Geography of Guam
Izu–Ogasawara Trench
Japanese archipelago
Mariana Islands
Mariana Trench
Mount Asama
Mount Ōyama (Kanagawa)
Back-arc regionBonin_IslandsBoso Triple JunctionBroadfin sawtail catsharkCongriscus megastomusDeepwater stingrayEsmeralda BankGeography_of_JapanGeology of the Pacific OceanGeothermal power in JapanHomeryonHoplostethus crassispinusIBM (disambiguation)Index of Northern Mariana Islands-related articlesIzu-Bonin-Mariana ArcIzu-Bonin ArcIzu-Ogasawara ArcIzu IslandsIzu–Bonin–Mariana ArcJapan TrenchJapanese submarine tender KomahashiKyushu-Palau RidgeKyushu–Palau RidgeList of large volcanic eruptionsList of submarine topographical featuresMariana Mud VolcanoesMariana PlateMariana TroughMount_FujiMyroconger gracilis
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Izu–Bonin–Mariana Arc
The Izu–Bonin–Mariana (IBM) arc system is a tectonic plate convergent boundary. The IBM arc system extends over 2800 km south from Tokyo, Japan, to beyond Guam, and includes the Izu Islands, the Bonin Islands, and the Mariana Islands; much more of the IBM arc system is submerged below sealevel. The IBM arc system lies along the eastern margin of the Philippine Sea Plate in the Western Pacific Ocean. It is the site of the deepest gash in Earth's solid surface, the Challenger Deep in the Mariana Trench.
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The Izu–Bonin–Mariana (IBM) ar ...... important ore deposits formed.
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January 2020
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The Izu–Bonin–Mariana (IBM) ar ...... er Deep in the Mariana Trench.
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Izu–Bonin–Mariana Arc
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