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  2. Philippine Sea - Wikipedia

    en.wikipedia.org/wiki/Philippine_Sea

    The Philippine Sea is a marginal sea of the Western Pacific Ocean east of the Philippine Archipelago ... Island arcs, which are actually ... This alters the water's ...

  3. Island arc - Wikipedia

    en.wikipedia.org/wiki/Island_arc

    Island arcs are long chains of active volcanoes with intense seismic ... This water is released during the ... Philippine Sea Plate Philippine Islands:

  4. Izu–Bonin–Mariana arc - Wikipedia

    en.wikipedia.org/wiki/Izu–Bonin–Mariana_Arc

    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

  5. North Luzon Trough - Wikipedia

    en.wikipedia.org/wiki/North_Luzon_Trough

    It is a well-developed forearc basin formed in front of the Luzon Volcanic Arc, an island arc system. [2] The trough is a result of the active subduction of the Philippine Sea Plate beneath the Eurasian Plate.

  6. Izu–Ogasawara Trench - Wikipedia

    en.wikipedia.org/wiki/Izu–Ogasawara_Trench

    Here, the Pacific plate is being subducted beneath the Philippine Sea plate, creating the Izu Islands and Bonin Islands on the Izu–Bonin–Mariana Arc system. [ 3 ] It is 9,826 metres (32,238 ft) +/- 11m at its deepest point and first dived to its base on August 13, 2022, during a joint Caladan Oceanic/University of Western Australia ...

  7. Mariana plate - Wikipedia

    en.wikipedia.org/wiki/Mariana_Plate

    The ]]Mariana Trough]] is located on the western side of the island arc along with the back arc basin. Around 3 Ma the basin began spreading at 4.7 cm/yr. [6] Due to the back arc spreading in the Mariana Trough the islands are moving east while the Philippine Sea plate is staying almost stationary. [4]

  8. Bicol Volcanic Arc - Wikipedia

    en.wikipedia.org/wiki/Bicol_Volcanic_Arc

    The Bicol Volcanic Arc is formed by the subduction of the Philippine Sea Plate beneath the Luzon Island Arc. As the Philippine Sea Plate descends beneath Luzon, it melts and releases fluids that rise through the overlying crust. These fluids, which are rich in silica, aluminum, and other minerals, eventually cool and solidify, forming the ...

  9. Ryukyu Arc - Wikipedia

    en.wikipedia.org/wiki/Ryukyu_Arc

    The Ryukyu Arc is an island arc which extends from the south of Kyushu along the Ryukyu Islands to the northeast of Taiwan, spanning about 1,200 kilometres (750 mi). [2] [3] [4] It is located along a section of the convergent plate boundary where the Philippine Sea Plate is subducting northwestward beneath the Eurasian Plate along the Ryukyu ...