Twelve or so plates slide over a partially molten lithosphere, and the continents, embedded in some of the plates, are carried by them. Where plates collide, mountains such as the [[Himalayas]] or the [[Rocky Mountains]] are formed. In some places, called subduction zones, one plate sinks beneath another plate and returns to the molten regions of the athenosphere. Along mid-oceanic ridges magma emerges to expand the plate and create new sea floor. | Twelve or so plates slide over a partially molten lithosphere, and the continents, embedded in some of the plates, are carried by them. Where plates collide, mountains such as the [[Himalayas]] or the [[Rocky Mountains]] are formed. In some places, called subduction zones, one plate sinks beneath another plate and returns to the molten regions of the athenosphere. Along mid-oceanic ridges magma emerges to expand the plate and create new sea floor. |