Here's why:
* Convection currents in the mantle: The Earth's mantle is constantly moving due to heat from the core. This movement creates convection currents that drag the tectonic plates along with them.
* Plate boundaries: The interaction between plates at their boundaries determines their movement.
* Divergent boundaries: Plates move apart (like at the Mid-Atlantic Ridge) creating new crust.
* Convergent boundaries: Plates collide, one often subducting under the other (like the Andes Mountains).
* Transform boundaries: Plates slide past each other (like the San Andreas Fault).
Think of it like a giant puzzle: Each plate piece is moving in its own way, bumping into, pulling apart, or sliding past its neighbors.
Key takeaway: The movement of tectonic plates is dynamic and complex, not a single, uniform direction.