The outer core is a significant layer of Earth, found between the mantle and the inner core. It is approximately 2200 km thick and is primarily composed of liquid iron and nickel, allowing it to flow freely. The movements within the outer core generate the Earth's magnetic field via a process known as the dynamo effect, which is fundamental in shielding the planet from solar radiation and maintaining life. The temperature in this layer can reach astonishing highs of up to 5000°C, further highlighting its dynamic and energetic nature. Understanding the outer core is crucial for grasping many geological and geophysical phenomena, including the mechanics behind the magnetic fields that influence navigational systems on Earth.