At the hottest point, the core inner core of the Earth is about 12500 degrees Fahrenheit due to radioactive materials that are constantly heating the Earth, just like a star.
Temperatures in the star's core can reach 3x109 K.
The Earth's core can reach temperatures of approximately 4,000 to 7,000 degrees Celsius (7,200 to 12,600 degrees Fahrenheit). This extreme heat is primarily due to the decay of radioactive isotopes and the pressure from the overlying layers of the Earth. The outer core is liquid, while the inner core is solid, despite these high temperatures, due to the immense pressure that prevents it from melting.
The earth's core can reach up to roughly about 2000 or 5000 degrees Celsius.
The hottest part of Earth's core is the inner core, which is primarily composed of iron and nickel. Temperatures in the inner core can reach up to 5,700 degrees Celsius (about 10,300 degrees Fahrenheit), making it hotter than the surface of the sun. The intense pressure at this depth keeps the inner core solid despite these extreme temperatures.
mantle is the thick layer before you reach the core of the earth
A convection cell.
No animal living on earth can survive the temperatures in the earths core. The temperature is between 5000-9000 degrees.
The Earth's core is mainly made of iron and nickel. The outer core is liquid, while the inner core is solid, due to high pressures and temperatures.
The interior core contains many nuclear properties which gives of huge amounts of heat which then heats the core.
The core of the Earth is hotter than lighting. The temperature of Earth's core can reach up to 5700°C, whereas lightning can reach temperatures of around 30,000°C.
Earth's core
made up of two layers composed of iron and nickel at very high temperatures