When tectonic plates collide and the direction of the forces is primarily perpendicular, the plates push up forming a mountain. The Himalayan Mountains are formed by the collision of two plates and are still growing. The summit of Mount Everest is, in fact, marine limestone.
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A subduction zone is formed at the bottom of the ocean where two plates collide. This is where one tectonic plate is forced beneath the other into the Earth's mantle, leading to the formation of deep ocean trenches and volcanic arcs.
A subduction zone is formed when two tectonic plates collide and one plate is forced beneath the other into the Earth's mantle. This process creates deep ocean trenches, volcanic arcs, and seismic activity.
Mountains and deep ocean trenches are two landforms that are created when tectonic plates collide. Mountains are formed when two continental plates collide and push against each other, while deep ocean trenches occur when one oceanic plate subducts beneath another.
A subduction zone is formed where two oceanic plates collide. One plate is forced beneath the other, creating a deep trench and often leading to volcanic activity and earthquakes.
When two oceanic plates collide, a deep ocean trench is formed due to one plate being pushed under the other in a process known as subduction. This subduction zone can create volcanic activity and earthquakes in the region.