Temperature, Pressure, and Density of the Interior of Earth
Temperature
The rise of temperature is often found in mines and deep wells. Along with this, the molten lava supports the fact that temperature increases towards the center of the earth. The rate of increase in temperature is not always uniform. It is mostly faster in some places and not so in others. Thus, it is mostly assumed that the rate of increase of temperature beneath surface is decreasing towards the center. The temperature of the center is 3000°C to 5000°C, Mostly due to chemical reactions under high-pressure situations.
Pressure
Pressure, as same as the temperature is increasing towards the center of the earth. This is mostly due to the weight of the overlying materials.
Density
Due to the increase in pressure and the presence of heavier materials towards the center, the density of the earth also increases towards the center.
Interior of the Earth
The interior of the earth is divided into three layers- Crust, Mantle, and Core. Crust refers to the outermost layer of the earth, the mantle is the portion of the interior beyond the crust and Core refers to the innermost layer of the earth.
Table of Content
- Interior of the Earth
- Crust
- Mantle
- Core
- Sources about Interior of the Earth
- Temperature, Pressure, and Density of the Interior of Earth
Interior of Earth
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