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  2. Island arc - Wikipedia

    en.wikipedia.org/wiki/Island_arc

    Most island arcs originate on oceanic crust and have resulted from the descent of the lithosphere into the mantle along the subduction zone. They are the principal way by which continental growth is achieved. [1] The Ryukyu Islands form an island arc. Island arcs can either be active or inactive based on their seismicity and presence of ...

  3. Convergent boundary - Wikipedia

    en.wikipedia.org/wiki/Convergent_boundary

    Volcanic arcs can form as island arc chains or as arcs on continental crust. Three magma series of volcanic rocks are found in association with arcs. The chemically reduced tholeiitic magma series is most characteristic of oceanic volcanic arcs, though this is also found in continental volcanic arcs above rapid subduction (>7 cm/year).

  4. Volcanic arc - Wikipedia

    en.wikipedia.org/wiki/Volcanic_arc

    A volcanic arc (also known as a magmatic arc [1]: 6.2 ) is a belt of volcanoes formed above a subducting oceanic tectonic plate, [2] with the belt arranged in an arc shape as seen from above. Volcanic arcs typically parallel an oceanic trench , with the arc located further from the subducting plate than the trench.

  5. 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 ...

  6. Scotia Arc - Wikipedia

    en.wikipedia.org/wiki/Scotia_Arc

    Bathymetry of the Scotia Arc. The Scotia Arc is the island arc system forming the north, east and south border of the Scotia Sea.The northern border, the North Scotia Ridge, comprises (from west to east): Isla de los Estados at the tip of Tierra del Fuego, the Burdwood, Davis, and Aurora Banks; the Shag, South Georgia Island and Clerke Rocks.

  7. Izu–Bonin–Mariana arc - Wikipedia

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

    The Izu–Bonin–Mariana (IBM) arc system is a tectonic plate convergent boundary in Micronesia.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.

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    Get AOL Mail for FREE! Manage your email like never before with travel, photo & document views. Personalize your inbox with themes & tabs. You've Got Mail!

  9. Oceanic trench - Wikipedia

    en.wikipedia.org/wiki/Oceanic_trench

    They are found on the oceanward side of island arcs and Andean-type orogens. [3] Globally, there are over 50 major ocean trenches covering an area of 1.9 million km 2 or about 0.5% of the oceans. [ 4 ]