volcanoes in an island arc
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.
When two continental plates collide,fold mountains are formed.
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.
when two oceanic plates collide they create a deep-ocean trench, at deep-ocean trenches subduction occurs.
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The surface feature formed when two plates meet is known as a fault. In some cases mountains can also be formed when two plates collide.
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volcanoes in an island arc
That is called subduction.
A mountain range forms when two of Earth's plates collide. The intense pressure and forces created by the collision push the Earth's crust upwards, creating towering peaks and ranges. Examples include the Himalayas formed by the collision of the Indian Plate and the Eurasian Plate.
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.