Starting from Earth's center, the layers of the Earth are as follows:
1. Inner Core: This is the innermost layer of the Earth, consisting mainly of solid iron and nickel. It is incredibly hot, with temperatures reaching up to 5,700 degrees Celsius.
2. Outer Core: Surrounding the inner core, the outer core is also composed of iron and nickel but in a liquid state. The movement of the molten outer core is responsible for generating Earth's magnetic field.
3. Mantle: Above the outer core lies the mantle, which is predominantly made up of solid rock containing silicate minerals. The mantle is divided into the upper mantle and the lower mantle.
4. Crust: The outermost layer of the Earth is the crust, which is a thin, solid shell that surrounds the planet. The Earth's crust is divided into oceanic crust, found beneath the oceans, and continental crust, which forms the continents.
By understanding the composition and characteristics of each layer, we can grasp the complex structure of the Earth and how these layers interact to support life on our planet.
