The lithosphere is the outermost layer of the Earth, consisting of the crust and the uppermost part of the mantle. It is a solid, brittle layer that varies in thickness and is divided into tectonic plates that float on the semi-fluid asthenosphere.
The lithosphere is primarily composed of rocky materials, including various types of minerals, rocks, and soil. The crust is made up of lighter, less dense rocks such as granite and basalt, while the upper mantle consists of denser rocks like peridotite.
The lithosphere is not a uniform layer, as it is divided into several tectonic plates that are in constant motion due to the underlying convection currents in the asthenosphere. These plates interact at their boundaries, leading to processes such as earthquakes, volcanic activity, and mountain building.