The pressure created by moving plates forces magma up through Earth's crust, forming mountains.
Mountains form where two continental plates collide. on account that both plates have a similar thickness and weight, neither one will sink under the alternative. rather, they fall down and fold till the rocks are forced as much as shape a mountain variety. as the plates keep to collide, mountains will get taller and taller.
A convergent plate boundary takes place whilst two plates push towards every different. when the plates collide the less dense plate overrides the denser plate, this is called subduction.
The crust on the plate this is pushed below is subjected to the excessive temperatures of the mantle under and the crust melts. as the vintage crust melts, volcanoes shape.
Plate edges are tough and two edges can get caught together even as the rest of the plate keeps moving.
subsequently, while the plate has moved far sufficient, the edges unstick and an earthquake occurs.
3/4 of all earthquakes occur at convergent limitations.
Many mountain degrees arise alongside these traces because while one plate doesn't completely move under the other, the earth crumbles and this uplifts the crust into mountains.
In Europe, the Alps are formed from the African and Eurasian plate bumping into each different.
As you fall, it pulls you toward the earth, or in the case of cliff diving, toward the water, at a speed of 32 feet per second per second (9.8 meters per second per second).
