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The {{Nihongo|'''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.<ref>{{cite web | authorlink = 沖繩縣文化環境部自然保護課 | title = Nature in Okinawa | publisher =沖繩縣 | url = http://www.pref.okinawa.lg.jp/site/kankyo/shizenhogo/hogo/documents/p1-7.pdf | accessdate = 2012-09-30 }}</ref> It comprises the entirety of the [[Ryukyu Islands]] chain. The Ryukyu and [[Southwest Honshu arc]]s together form the southwest trending arm of the [[triple junction]].
The {{Nihongo|'''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.<ref>{{cite web | authorlink = 沖繩縣文化環境部自然保護課 | title = Nature in Okinawa | publisher =沖繩縣 | url = http://www.pref.okinawa.lg.jp/site/kankyo/shizenhogo/hogo/documents/p1-7.pdf | accessdate = 2012-09-30 }}</ref> It comprises the entirety of the [[Ryukyu Islands]] chain. The Ryukyu and [[Southwest Honshu arc]]s together form the southwest trending arm of the [[Boso Triple Junction]].


==Major islands==
==Major islands==

Revision as of 04:48, 9 October 2012

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 Boso Triple Junction.

Major islands

Nansei Islands (南西諸島, Nansei-shotō)

References

  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.