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  2. Makran Trench - Wikipedia

    en.wikipedia.org/wiki/Makran_Trench

    The Makran Subduction Zone is often split into two segments: the east and west. The Sonne fault divides the two. [3] Though largely much quieter than many other subduction zones, studies reveal that the Makran Trench may be capable of very large earthquakes, even extending into the magnitude 9 range. [4]

  3. Subduction - Wikipedia

    en.wikipedia.org/wiki/Subduction

    The surface expressions of subduction zones are arc-trench complexes. On the ocean side of the complex, where the subducting plate first approaches the subduction zone, there is often an outer trench high or outer trench swell. Here the plate shallows slightly before plunging downwards, as a consequence of the rigidity of the plate. [18]

  4. Sagami Trough - Wikipedia

    en.wikipedia.org/wiki/Sagami_Trough

    Red line is the Sagami Trough. The Sagami Trough (相模トラフ, Sagami Torafu) also Sagami Trench, Sagami Megathrust, or Sagami Subduction Zone is a 340-kilometre (210 mi)long trough, which is the surface expression of the convergent plate boundary where the Philippine Sea plate is being subducted under the Okhotsk microplate.

  5. 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 .

  6. Convergent boundary - Wikipedia

    en.wikipedia.org/wiki/Convergent_boundary

    Oceanic trenches are narrow topographic lows that mark convergent boundaries or subduction zones. Oceanic trenches average 50 to 100 km (31 to 62 mi) wide and can be several thousand kilometers long. Oceanic trenches form as a result of bending of the subducting slab.

  7. Nankai Trough - Wikipedia

    en.wikipedia.org/wiki/Nankai_Trough

    In plate tectonics, the Nankai Trough marks a subduction zone that is caused by subduction of the Philippine Sea plate beneath Japan, part of the Eurasian plate (Kanda et al., 2004). This plate boundary would be an oceanic trench except for a high flux of sediments that fills the trench.

  8. Aleutian subduction zone - Wikipedia

    en.wikipedia.org/wiki/Aleutian_Subduction_Zone

    Here, the Pacific Plate is being subducted underneath the North American Plate and the rate of subduction changes from west to east from 7.5 to 5.1 cm (3.0 to 2.0 in) per year. [2] The Aleutian subduction zone includes two prominent features, the Aleutian Arc and the Aleutian Trench. The Aleutian Arc was created via volcanic eruptions from ...

  9. Category:Subduction zones - Wikipedia

    en.wikipedia.org/wiki/Category:Subduction_zones

    Pages in category "Subduction zones" The following 52 pages are in this category, out of 52 total. ... Negros Trench; New Britain subduction zone; New Britain Trench ...