why The moveable plates on the earth’s crust collide against each other.
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The plates can be thought of like pieces of a cracked shell that rest on the hot, molten rock of Earth's mantle and fit snugly against one another. The heat from radioactive processes within the planet's interior causes the plates to move, sometimes toward and sometimes away from each other.
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When mantle rocks are heated unevenly from below, most geologists believe that they can circulate in a cyclic fashion called "convection." Currently, some form of convection in the mantle is the most widely accepted mechanism for plate movement.
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