The Earth's lithoshpere is cracked into tectonic plates.
Intenses heat by radioactive decay deep inside the Earth, creates convection currents in the mantle. These currents cause the tectonic plates to move apart very slowly by only a few centimeters a year.
In convection in a gas or liquid, the matter rises as it is heated. As it gets further away from the heat source, it cools and sink. This is what is happening in the Earth.
1. Hot new molten rock rises to the surface,creating new crust
2.The older, cooler crust, then sinks down where the convection current starts to fall.
3. The land masses on these plates move very slowly.
The movements are usually small and gradual, but sometime they can be sudden and disastrous. Earthquakes and volcanic eruption are common occurances at plate boundries. They are hard to predict.
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