At which boundary do two continental plates collide to form tall mountain ranges like the Himalayas?

At which boundary do two continental plates collide to form tall mountain ranges like the Himalayas?

• A. Divergent Boundary
• B. Transform Boundary
• C. Convergent Boundary (Continental/Continental)
• D. Subduction Zone

Answer: (C)

When two continental plates collide at a convergent boundary, the crust is forced to buckle and thicken rather than sink. This collision squeezes the crust upward, building tall mountain ranges like the Himalayas. The Himalayas formed as the Indian Plate pushed into the Eurasian Plate, causing intense crustal deformation, folding, and uplift that created the soaring peaks and the high Tibetan Plateau. Divergent boundaries involve plates moving apart, leading to features such as rifts and mid-ocean ridges, not towering mountains. Transform boundaries are where plates slide past each other horizontally, causing earthquakes along faults but not major mountain uplift. Subduction zones occur when one plate sinks beneath another, often generating volcanic activity, which isn’t the mechanism behind these continental-continental mountains. So, the boundary responsible for forming such ranges is a convergent boundary with continental-continental collision.

When two continental plates collide at a convergent boundary, the crust is forced to buckle and thicken rather than sink. This collision squeezes the crust upward, building tall mountain ranges like the Himalayas. The Himalayas formed as the Indian Plate pushed into the Eurasian Plate, causing intense crustal deformation, folding, and uplift that created the soaring peaks and the high Tibetan Plateau.

Divergent boundaries involve plates moving apart, leading to features such as rifts and mid-ocean ridges, not towering mountains. Transform boundaries are where plates slide past each other horizontally, causing earthquakes along faults but not major mountain uplift. Subduction zones occur when one plate sinks beneath another, often generating volcanic activity, which isn’t the mechanism behind these continental-continental mountains.

So, the boundary responsible for forming such ranges is a convergent boundary with continental-continental collision.