Subduction zones form along some tectonic plate boundaries. Of the three general types of tectonic plate boundaries, we will see them form at some (but not all) of what are called convergent plate boundaries.
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Subduction zones form at convergent plate boundaries, where one tectonic plate is pushed beneath another into the Earth's mantle. This process can lead to the formation of deep oceanic trenches and volcanic arcs.
Convergent boundaries that produce maintains are called subduction zones.
A convergent boundary is formed when plates collide. At this type of boundary, the denser plate sinks beneath the less dense plate in a process known as subduction. This collision often results in the formation of mountain ranges, volcanoes, and deep ocean trenches.
At a converging boundary, plates can collide and create subduction zones. This can lead to the formation of mountain ranges, deep ocean trenches, and earthquakes. The pressure and friction from the plates can also cause volcanic activity.
Subduction zones form at convergent plate boundaries where one tectonic plate is forced beneath another plate. This process occurs when one plate is denser than the other, causing it to sink into the mantle and creating a subduction zone.
Both subduction zones and spreading centers.