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A subduction zone is an area of tectonic plate collision where the more dense plate subducts, or follows a path underneath, the less dense plate.

A subduction zone is the place where oceanic plate margin is being pushed under a continental plate or a less dense oceanic plate. Have a look at the western side of South America (on the pacific coast), see the mountain ranges and volcanoes - these are just inside the edge of the continental plate and are a product of the subduction zone. As oceanic crust gets pushed under or over-ridden by the continental plate edge it melts and gives rise to the volcanoes. These zones also exist where one oceanic crust is pushed under another oceanic crust, the same volcanism results, but as it takes place at sea the result is the formation of underwater volcanoes.

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