Our planet, Earth, is composed of several distinct layers that vary in composition and function.
- The outermost layer is the **crust**, which is where we live and consists of solid rocks.
- Beneath the crust lies the **mantle**, a massive layer with semi-solid rock that varies from rigid to malleable.
- Below the mantle, we find the **outer core**, which is mainly liquid and composed of iron and nickel.
- The center of the Earth is the **inner core**, a dense ball of solid metal.
Itβs fascinating how each of these layers plays a significant role in Earth's geology. For example, the movement and behavior of these layers are crucial for understanding phenomena like earthquakes and volcanic activity.
These layers are dynamically interacting with each other, and together, they form the very structure of our planet.