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  2. Subduction - Wikipedia

    en.wikipedia.org/wiki/Subduction

    An example of a volcanic arc having both island and continental arc sections is found behind the Aleutian Trench subduction zone in Alaska. Volcanoes that occur above subduction zones, such as Mount St. Helens, Mount Etna, and Mount Fuji, lie approximately one hundred kilometers from the trench in arcuate chains called volcanic arcs.

  3. Tonga–Kermadec Ridge - Wikipedia

    en.wikipedia.org/wiki/Tonga–Kermadec_Ridge

    It is a result of the most linear, fastest converging, and seismically active subduction boundary on Earth, the Kermadec–Tonga subduction zone, and consequently has the highest density of submarine volcanoes. [1] The Tonga–Kermadec Ridge stretches more than 3,000 km (1,900 mi) north-northeast from New Zealand's North Island.

  4. Kermadec–Tonga subduction zone - Wikipedia

    en.wikipedia.org/wiki/Kermadec–Tonga_subduction...

    The Kermadec–Tonga subduction zone is a convergent plate boundary that stretches from the North Island of New Zealand northward. The formation of the Kermadec and Tonga plates started about 4–5 million years ago. Today, the eastern boundary of the Tonga plate is one of the fastest subduction zones, with a rate up to 24 cm/year (9.4 in/year ...

  5. Cascadia subduction zone - Wikipedia

    en.wikipedia.org/wiki/Cascadia_subduction_zone

    The Cascadia subduction zone is a 960 km (600 mi) fault at a convergent plate boundary, about 100–200 km (70–100 mi) off the Pacific coast, that stretches from northern Vancouver Island in Canada to Northern California in the United States

  6. Cascade Volcanoes - Wikipedia

    en.wikipedia.org/wiki/Cascade_Volcanoes

    However, in common with most other subduction zones, the outer margin is slowly being compressed, similar to a giant spring. When the stored energy is suddenly released by slippage across the fault at irregular intervals, the Cascadia subduction zone can create very large earthquakes such as the M w 8.7–9.2 Cascadia earthquake of 1700.

  7. Volcanic arc - Wikipedia

    en.wikipedia.org/wiki/Volcanic_arc

    A volcanic arc is part of an arc-trench complex, which is the part of a subduction zone that is visible at the Earth's surface. A subduction zone is where a tectonic plate composed of relatively thin, dense oceanic lithosphere sinks into the Earth's mantle beneath a less dense overriding plate. The overriding plate may be either another oceanic ...

  8. Aleutian subduction zone - Wikipedia

    en.wikipedia.org/wiki/Aleutian_Subduction_Zone

    The Aleutian subduction zone includes two prominent features, the Aleutian Arc and the Aleutian Trench. The Aleutian Arc was created via volcanic eruptions from dehydration of the subducting slab at ~100 km depth.

  9. Vanuatu subduction zone - Wikipedia

    en.wikipedia.org/wiki/Vanuatu_subduction_zone

    The Vanuatu subduction zone (previously called New Hebrides subduction zone) is currently one of the most active subduction zones on Earth, producing great earthquakes (magnitude 8.0 or greater), with potential for tsunami hazard to all coastlines of the Pacific Ocean. [2] [3] There are active volcanoes associated with arc volcanism.