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  2. Subduction - Wikipedia

    en.wikipedia.org/wiki/Subduction

    Plutons, like Half Dome in Yosemite National Park, generally form 10–50 km [65] below the volcanoes within the volcanic arcs and are only visible on the surface once the volcanoes have weathered away. The volcanism and plutonism occur as a consequence of the subducting oceanic slab dehydrating as it reaches higher pressures and temperatures.

  3. Volcanic arc - Wikipedia

    en.wikipedia.org/wiki/Volcanic_arc

    The magma ascends to form an arc of volcanoes parallel to the subduction zone. Volcanic arcs are distinct from volcanic chains formed over hotspots in the middle of a tectonic plate. Volcanoes often form one after another as the plate moves over the hotspot, and so the volcanoes progress in age from one end of the chain to the other.

  4. List of tectonic plate interactions - Wikipedia

    en.wikipedia.org/wiki/List_of_tectonic_plate...

    Subduction zones are marked by oceanic trenches. The descending end of the oceanic plate melts and creates pressure in the mantle, causing volcanoes to form. Back-arc basins can form from extension in the overriding plate, in response to the displacement of the subducting slab at some oceanic trenches. This paradoxically results in divergence ...

  5. Volcano - Wikipedia

    en.wikipedia.org/wiki/Volcano

    When it does reach the surface, however, a volcano is formed. Thus subduction zones are bordered by chains of volcanoes called volcanic arcs. Typical examples are the volcanoes in the Pacific Ring of Fire, such as the Cascade Volcanoes or the Japanese Archipelago, or the eastern islands of Indonesia. [16] [2]

  6. Cascade Volcanoes - Wikipedia

    en.wikipedia.org/wiki/Cascade_Volcanoes

    The arc formed due to subduction along the Cascadia subduction zone. Although taking its name from the Cascade Range , this term is a geologic grouping rather than a geographic one, and the Cascade Volcanoes extend north into the Coast Mountains , past the Fraser River which is the northward limit of the Cascade Range proper.

  7. 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 ...

  8. Aleutian subduction zone - Wikipedia

    en.wikipedia.org/wiki/Aleutian_Subduction_Zone

    The Aleutian island arc formed ~50-55 ma as a result of Kula Plate subduction under the North American Plate before the Pacific plate arrived. [3] There are three stratigraphic units of the Aleutian island arc: volcanic rocks from ~55-33 ma, marine sedimentary rocks from ~23-33 ma, and sedimentary and igneous rocks from ~5 ma-present. [3]

  9. Category:Subduction volcanoes - Wikipedia

    en.wikipedia.org/wiki/Category:Subduction_volcanoes

    Pages in category "Subduction volcanoes" The following 200 pages are in this category, out of approximately 305 total. This list may not reflect recent changes .