The Earth's crust forms the outermost shell of our planet. It is relatively thin compared to other layers and can be classified into two types: continental and oceanic crust.
The continental crust is thicker, ranging between 30 to 70 kilometers, and mostly composed of light-colored, granitic rocks. The oceanic crust, on the other hand, is thinner, about 5 to 10 kilometers thick, and primarily made up of dark, basaltic rocks.
- The crust is where we live and is critical for supporting life, providing essential resources like minerals and soil.
- It is also the place where tectonic activity occurs, such as earthquakes and volcanic eruptions.
Understanding the Earth's crust helps us learn about the dynamic processes of our planet and how they shape the environment.