Which feature results from colliding plates that compress and uplift rocks to form mountains?

Which feature results from colliding plates that compress and uplift rocks to form mountains?

• A. Divergent Boundaries
• B. Convergent Boundaries
• C. Collision Zones
• D. Subduction Zones

Answer: (C)

When two continental plates collide, the edges crumple and the crust thickens, pushing rocks upward to form mountain ranges. This uplift happens in collision zones, where the compression from the converging plates thickens and deforms the crust to create tall, rugged landscapes. Divergent boundaries move plates apart, which tends to produce rift valleys and new crust rather than mountain uplift. Subduction zones involve one plate sliding beneath another, leading to trenches and volcanic activity rather than the large-scale uplift of continental crust. While convergent boundaries describe plates coming together, the specific feature that builds mountains from continental collision is the collision zone, as seen in examples like the Himalayas formed by the Indian and Eurasian plate collision.

When two continental plates collide, the edges crumple and the crust thickens, pushing rocks upward to form mountain ranges. This uplift happens in collision zones, where the compression from the converging plates thickens and deforms the crust to create tall, rugged landscapes. Divergent boundaries move plates apart, which tends to produce rift valleys and new crust rather than mountain uplift. Subduction zones involve one plate sliding beneath another, leading to trenches and volcanic activity rather than the large-scale uplift of continental crust. While convergent boundaries describe plates coming together, the specific feature that builds mountains from continental collision is the collision zone, as seen in examples like the Himalayas formed by the Indian and Eurasian plate collision.