The core is the innermost layer of the Earth, located beneath the mantle. It is made up of two parts: the inner core and the outer core.
The inner core is solid and consists mainly of iron and nickel. It has a temperature of about 5,700°C to 7,000°C. The immense pressure at the center of the Earth keeps the inner core in a solid state, despite the high temperatures.
The outer core is a liquid layer composed of molten iron and nickel. It is responsible for generating the Earth's magnetic field through the movement of the molten metals. This magnetic field protects the Earth from solar winds and cosmic radiation.
The core plays a crucial role in the Earth's structure and processes. Its heat contributes to the movement of tectonic plates, which leads to phenomena such as earthquakes and volcanic eruptions. Additionally, the magnetic field generated by the outer core protects the Earth's atmosphere and helps sustain life on our planet.