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  2. Oceanic trench - Wikipedia

    en.wikipedia.org/wiki/Oceanic_trench

    Oceanic crust is formed at an oceanic ridge, while the lithosphere is subducted back into the asthenosphere at trenches. Oceanic trenches are prominent, long, narrow topographic depressions of the ocean floor. They are typically 50 to 100 kilometers (30 to 60 mi) wide and 3 to 4 km (1.9 to 2.5 mi) below the level of the surrounding oceanic ...

  3. Category:Oceanic trenches by sea or ocean - Wikipedia

    en.wikipedia.org/wiki/Category:Oceanic_trenches...

    Category: Oceanic trenches by sea or ocean. 7 languages. ... Download as PDF; Printable version; In other projects Wikidata item; Appearance. move to sidebar hide. Help

  4. Category:Oceanic trenches - Wikipedia

    en.wikipedia.org/wiki/Category:Oceanic_trenches

    Download as PDF; Printable version; In other projects ... Pages in category "Oceanic trenches" The following 6 pages are in this category, out of 6 total.

  5. Marine geology - Wikipedia

    en.wikipedia.org/wiki/Marine_geology

    At the deepest point, the trench is nearly 11,000 m deep (almost 36,000 feet). [38] [3] This is further below sea level than Mount Everest is above sea level, by over 2 kilometers. Volcanic arcs and oceanic trenches partly encircling the Pacific Basin form the so-called Pacific Ring of fire, a zone of frequent earthquakes and volcanic eruptions.

  6. List of submarine topographical features - Wikipedia

    en.wikipedia.org/wiki/List_of_submarine...

    An oceanic trench is a type of convergent boundary at which two oceanic lithospheric slabs meet; the older (and therefore denser) of these slabs flexes and subducts beneath the other slab. Oceanic lithosphere moves into trenches at a global rate of about a tenth of a square meter per second.

  7. Outline of plate tectonics - Wikipedia

    en.wikipedia.org/wiki/Outline_of_plate_tectonics

    The relative movement of the plates typically ranges from zero to 10 cm annually. Faults tend to be geologically active, experiencing earthquakes, volcanic activity, mountain-building, and oceanic trench formation. Tectonic plates are composed of the oceanic lithosphere and the thicker continental lithosphere, each topped by its own kind of crust.

  8. Forearc - Wikipedia

    en.wikipedia.org/wiki/Forearc

    Initial theories proposed that the oceanic trenches and magmatic arcs were the primary suppliers of the accretionary sedimentation wedges in the forearc regions. More recent discovery suggests that some of the accreted material in the forearc region is from a mantle source along with trench turbidites derived from continental material. This ...

  9. Vityaz Trench - Wikipedia

    en.wikipedia.org/wiki/Vityaz_Trench

    The approxiamate area of deep-focus earthquakes mentioned in the page text that may be associated with the old subduction at the trench is shaded light red. The Vityaz Trench (also known as the Vitiaz or East Melanesian Trench [ 1 ] ) is an oceanic trench tectonic feature of the South West Pacific Ocean floor.