* Continuously Moving: Tectonic plates are constantly moving, colliding, separating, and sliding past each other.
* Plate Boundaries: Where these plates interact, we find major geological features like mountain ranges, volcanoes, and earthquakes.
* Subduction: One plate can dive under another (subduction) which can change the size and number of plates over very long periods.
Major Plates:
We usually talk about 7 or 8 major tectonic plates:
* African Plate
* Antarctic Plate
* Eurasian Plate
* Indo-Australian Plate
* North American Plate
* Pacific Plate
* South American Plate
Smaller Plates:
There are also numerous smaller plates, sometimes called "microplates", that exist alongside the major ones.
Constantly Evolving:
The Earth's tectonic system is a very complex and dynamic process. The number of plates and their boundaries are always shifting and evolving over geological time scales.