The Earth's core is a hot, dense, metallic ball composed primarily of iron and nickel. It is divided into two distinct regions: the outer core and the inner core.
The outer core is a liquid layer that surrounds the inner core. It is composed of molten iron and nickel and is responsible for generating the Earth's magnetic field through the movement of these metallic fluids.
The inner core is a solid, dense sphere with a radius of about 1,220 kilometers. It is under immense pressure, which causes the iron and nickel to be in a solid state despite the high temperatures. The inner core is thought to be as hot as the surface of the sun.
Research the latest scientific findings and theories about the Earth's core. Explore how advancements in technology have allowed scientists to study and understand the core more effectively.