Tectonic plates are large, rigid pieces of the Earth's lithosphere. They move and interact at their boundaries. There are several major tectonic plates, including the Pacific Plate, the North American Plate, and the Eurasian Plate.
These movements are driven by forces such as:
- Mantle convection: The flow of hot, molten rock in the mantle that causes plates to move.
- Slab pull: The force exerted by a sinking plate pulling the rest of the plate with it.
- Ridge push: The force that drives plates away from mid-ocean ridges where new crust is formed.
Plates can move apart, come together, or slide past each other. These interactions create many geological phenomena.