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The plates are bounded by three types of features A dense oceanic plate will be forced under a more buoyant plate (often a continental plate) and sinks into the mantle. Transform faults, where plates slide past one another

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And subduction zones, where plates overlap, with one plate sliding under the other. Volcano activity at subduction zone Aside from the trenches and volcanic eruptions, subduction zones also cause earthquakes

When two massive crustal plates collide, the energy that is stored is also enormous.

Subduction zones are where earth’s tectonic plates collide and one plate plunges beneath another, driving volcanic arcs, powerful earthquakes, and profound geological transformations. Where they collide and one plate is thrust beneath another (a subduction zone), the most powerful earthquakes, tsunamis, volcanic eruptions, and landslides occur. Oceanic trench, volcanic arc, accretionary wedge, and descending slab into the mantle When an oceanic plate collides with a continental plate, the denser oceanic plate subducts beneath the lighter continental plate.

Subduction examples reveal the dramatic interactions between tectonic plates that create mountains, earthquakes, and volcanic activity Subduction zones are geological regions where one tectonic plate is forced beneath another, leading to significant geological activity, including earthquakes and volcanic eruptions. Subduction zones occur at convergent plate boundaries where two tectonic plates meet and one dives beneath the other