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Ryukyu arc

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The Ryukyu arc (琉球弧, Ryūkyū-ko) is a volcanic island arc system of Japan's triple junction formed by the subduction of the Phillipine plate beneath the Eurasian plate between Ryukyu Trench to the south-east and the Okinawa Trough to north-west.[1] It comprises the entirety of the Ryukyu Islands chain. The Ryukyu and Southwest Honshu arcs together form the southwest trending arm of the triple junction.


Major islands

Nansei Islands (南西諸島, Nansei-shotō)

Notes

  1. ^ "Nature in Okinawa" (PDF). 沖繩縣. Retrieved 2012-09-30.
  2. ^ "Global Volcanism Program | Iwo-Tori-shima | Summary". Volcano.si.edu. Retrieved 2012-10-07.