Subduction zones form between converging oceanic and continental plates, leading to trenches, earthquakes, and volcanic arcs.
Subduction zones are likely to form between converging oceanic and continental plates. In this process, the denser oceanic plate sinks beneath the lighter continental plate, leading to the formation of features like deep trenches, earthquakes, and volcanic arcs.
When oceanic and continental plates converge, subduction occurs, creating significant geological phenomena such as volcanic activity along coastlines. Examples of this can be seen in areas like the Pacific Ring of Fire, known for its intense volcanic and seismic activity.
Volcanic arcs and island chains often result from oceanic-oceanic subduction zones, where one oceanic plate subducts beneath another. This process leads to the formation of chains of volcanic islands, such as the Aleutian Islands and the Lesser Antilles.
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