ocean trench
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How ocean trenches and mid-ocean ridges are formed
Credit: U.S. Geological Survey
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A long, narrow, linear depression of the sea floor caused by the subduction
of one plate under another. Ocean trenches have a V-shaped cross-section
and run, typically, roughly parallel to continental coastal mountain ranges
or volcanic island arcs. See also mid-ocean
ridge. Related category
GEOLOGY
AND PLANETARY SCIENCE
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