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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 colliding, 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 plates bumping into each different.

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