The Earth's core is the innermost part of our planet. It is divided into two layers: the outer core and the inner core. The core is primarily composed of iron and nickel, with smaller amounts of other elements.
The outer core is a liquid layer that surrounds the inner core. It is about 2,200 kilometers thick and is responsible for generating Earth's magnetic field through the movement of molten iron and nickel.
The inner core is a solid sphere with a radius of about 1,220 kilometers. It experiences extremely high temperatures and pressures, causing the iron and nickel to exist in a solid state despite the intense heat.