The Eurasian and the Indian Plates collided to make Krakatoa (also known as Krakatau) erupt
mountains, crevasses, canyons
When two plates collide, it can form different geological features such as mountain ranges, deep-sea trenches, and volcanic arcs. The exact formations that occur depend on the type of collision, whether it's a convergent boundary where plates collide, or a transform boundary where plates slide past each other.
When two Continental plates collide, both plates lift upward and it can form mountains or mountain chains.
Mountain ranges are formed when two continental plates collide. When they converge one plate will be forced slightly under the other one.
When plates collide it is called a convergent boundary.newtest3
convergent boundary
Convergent boundary
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A convergent boundary is formed when plates collide. At this type of boundary, the denser plate sinks beneath the less dense plate in a process known as subduction. This collision often results in the formation of mountain ranges, volcanoes, and deep ocean trenches.
A convergent boundary is where two plates collide. This can lead to the formation of mountains, earthquakes, and volcanic activity.
When plates with edges which have ocean lithosphere collide with each other, one plate can be pushed under the other, causing the magma from the mantle to rise. This results in the formation volcanic mountains in the vicinity.
When plates collide, they can either crumple and fold, creating mountain ranges, or one plate can slide beneath the other, forming trenches and volcanic arcs. The type of collision depends on the type of plates involved - oceanic, continental, or a combination.