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The journey from the ground beneath our feet to the very heart of our planet is a vast distance, best approximated at 4,000 miles, or about 6,400 kilometers. Our planet isn't a perfect sphere; it's technically an oblate spheroid. This means it bulges slightly at the equator and is flatter at the poles due to its constant rotation. As a result, the distance to the center is slightly greater from the equator (about 3,963 miles) than it is from the North or South Pole (about 3,950 miles). The 4,000-mile figure represents a handy and close average of these different measurements.
Venturing through this immense distance would reveal a world of extreme conditions and distinct layers. The initial part of the journey would be through the Earth's crust, the relatively thin outer layer we live on. The crust's thickness varies, ranging from about five miles thick under the oceans to an average of 25 miles thick beneath the continents. Below the crust lies the mantle, which is the planet's thickest layer, making up about 84% of Earth's volume. This layer of hot, dense, flowing rock is approximately 1,800 miles (2,900 kilometers) thick.
After passing through the mantle, you would reach the core, which is separated into two parts. The outer core is a superheated liquid layer of iron and nickel about 1,400 miles thick. The movement within this liquid outer core is what generates Earth's protective magnetic field. At the very center lies the inner core, a solid ball of iron and nickel with a radius of about 759 miles. Despite temperatures as hot as the surface of the sun, the immense pressure at the center of the Earth prevents the inner core from melting.
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