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Answer:
When tectonic plates collide, several geological processes can occur depending on the nature of the collision:
Subduction: One plate is forced beneath another. This often forms deep ocean trenches and volcanic arcs. For example, the Pacific Plate is subducting beneath the North American Plate, creating the Cascade Range volcanoes.
Mountain Building: When two continental plates collide, they can push up mountain ranges. The Himalayas, formed by the collision of the Indian Plate with the Eurasian Plate, are a classic example.
Earthquakes: Collisions can cause stress to build up along faults, leading to earthquakes. These are common in collision zones and transform boundaries (where plates slide past each other).
Plate Boundary Features: Different types of plate boundaries, like convergent (colliding), divergent (moving apart), and transform (sliding past each other), each have characteristic features such as ridges, trenches, or faults.
In summary, plate collisions can lead to volcanic activity, mountain formation, earthquakes, and various geological features depending on the type of plates involved and their interactions.
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