The surface of the Earth, also known as the lithosphere, is divided into several large sections called tectonic plates. These plates are floating on a semi-fluid layer beneath them known as the asthenosphere. Because these plates are always in motion, driven by forces such as mantle convection, they interact with one another at their boundaries.
Some key characteristics of tectonic plates include:
- They vary in size and shape.
- Each plate can consist of both oceanic and continental crust.
- Plate movements can cause earthquakes, volcanic activity, and the creation of mountain ranges.
There are three types of plate boundaries: convergent, divergent, and transform. Mountain ranges like the Himalayas are primarily formed at convergent boundaries where plates collide and the crust is pushed upward.