The Earth's mantle is a very hot layer, and here are some facts about its heat:
Temperature Variation in the Mantle
The temperature within the Earth's mantle is not uniform, but rather increases with depth. This means that the deeper you go, the hotter it gets. The following are some temperature facts that are found in the reference:
- Near the Earth's crust, the mantle's temperature is approximately 1832 degrees Fahrenheit (1000 degrees Celsius).
- However, around the boundary where the lower mantle meets the outer core, the temperature rises significantly to about 6692 degrees Fahrenheit (3700 degrees Celsius).
Key Takeaways
- The mantle is a very hot layer of the Earth.
- There is a significant temperature difference from the top to bottom of the mantle.
- The Earth's interior temperature increases with depth.
- Mantle heat is the driving force behind many geological processes, such as plate tectonics.
