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  2. Subduction zone metamorphism - Wikipedia

    en.wikipedia.org/wiki/Subduction_zone_metamorphism

    Subduction zones host a unique variety of rock types formed by the high-pressure, low-temperature conditions a subducting slab encounters during its descent. [4] The metamorphic conditions the slab passes through in this process generates and alters water bearing (hydrous) mineral phases, releasing water into the mantle.

  3. Tonga–Kermadec subduction zone - Wikipedia

    en.wikipedia.org/wiki/Tonga–Kermadec_subduction...

    With the largest underwater volcano chain, the region surrounding the Tonga–Kermadec subduction zone is one of the most geologically diverse areas in the world. [7] The Kermadec Sanctuary was proposed in 2015 by the Prime Minister of New Zealand, John Key , at the United Nations in New York, which would create an area off limits to ...

  4. Subduction - Wikipedia

    en.wikipedia.org/wiki/Subduction

    Subduction zone physics: Sinking of the oceanic lithosphere (sediments, crust, mantle), by the contrast of density between the cold and old lithosphere and the hot asthenospheric mantle wedge, is the strongest force (but not the only one) needed to drive plate motion and is the dominant mode of mantle convection. [citation needed]

  5. 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 ...

  6. 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

  7. Marine geology - Wikipedia

    en.wikipedia.org/wiki/Marine_geology

    Each boundary type is associated with different geological marine features. Divergent plates are the cause for mid-ocean ridge systems while convergent plates are responsible for subduction zones and the creation of deep ocean trenches. Transform boundaries cause earthquakes, displacement of rock, and crustal deformation. [8] [27] [26] [28]

  8. Manila Trench - Wikipedia

    en.wikipedia.org/wiki/Manila_Trench

    The NFZ has many normal faults, often covered by the trench fill sediments. This zone has thought to have been formed by the bending of the lithosphere resulting from subduction processes (causing gravity sliding and faulting). [17] The PTZ represents the transitional zone between the extensional and compressional environments along the Manila ...

  9. Flat slab subduction - Wikipedia

    en.wikipedia.org/wiki/Flat_Slab_Subduction

    The subduction of bathymetric highs such as aseismic ridges, oceanic plateaus, and seamounts has been posited as the primary driver of flat slab subduction. [3] The Andean flat slab subduction zones, the Peruvian slab and the Pampean (Chilean) flat slab, are spatially correlated with the subduction of bathymetric highs, the Nazca Ridge and the Juan Fernandéz Ridge, respectively.

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