Subduction zones occur where oceanic plates subduct beneath continental plates, forming volcanic arcs and triggering earthquakes.
Subduction zones form where oceanic plates collide with continental plates, resulting in the oceanic plate being forced beneath the continental plate. A notable feature of this interaction is the formation of a volcanic arc, seen in regions like the Cascade Range and the Andes Mountains.
Earthquakes are common in these subduction zones and can lead to tsunamis. The depth of the zones varies, and valuable minerals can be created due to magmatic activity.
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