lithosfären

The lithosphere is the outermost shell of the Earth, comprising the crust and the uppermost part of the mantle. It is divided into several tectonic plates that float on the more fluid asthenosphere below. The lithosphere is approximately 100 kilometers thick, although this thickness varies depending on the location and the type of crust. The crust, which is the outermost layer, is further divided into oceanic and continental crust. Oceanic crust is thinner and denser, while continental crust is thicker and less dense. The lithosphere is a critical component of plate tectonics, the theory that explains the movement and interaction of these tectonic plates. This movement is responsible for various geological phenomena, such as earthquakes, volcanic activity, and the formation of mountain ranges. The lithosphere also plays a significant role in the Earth's climate and weather patterns, as it influences the distribution of heat and moisture across the planet. Despite its importance, the lithosphere remains a subject of ongoing scientific research, with many aspects of its behavior and composition still not fully understood.