The temperature at the center of the Earth is estimated to be around 5,000 to 7,000 degrees Celsius (about 9,000 to 13,000 degrees Fahrenheit).
This incredibly high temperature is due to several factors. First, the Earth’s core is primarily made of iron and nickel, which have high melting points. The immense pressure at the center of the Earth also contributes to the high temperatures, as pressure can raise the melting point of materials.
Additionally, heat is generated in the core through the decay of radioactive isotopes and the residual heat from the planet’s formation. This combination of pressure and radioactive decay keeps the core in a molten state and creates a significant amount of heat. Understanding the temperature of the Earth’s center helps geologists comprehend the dynamics of the planet’s interior and the processes that drive plate tectonics and volcanic activity.