The Earth's core is the innermost part of the Earth, located below the mantle. It is divided into two main parts: the inner core and the outer core.
The inner core is a solid sphere made primarily of iron and nickel. It is extremely hot, with temperatures reaching up to 9,000 degrees Fahrenheit. The immense pressure from the layers above keeps the inner core in a solid state despite the high temperatures.
The outer core is a liquid layer also made of iron and nickel. It surrounds the inner core and is responsible for generating the Earth's magnetic field through the movement of molten metal. This movement, known as convection, creates electric currents that produce the magnetic field that protects the Earth from solar winds and cosmic radiation.
Understanding the Earth's core is crucial in comprehending the dynamics of the Earth's internal structure and its influence on the planet's magnetic field and geological processes.