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Iron, nickel, oxygen, silicon, hydrogen, and carbon are believed to have formed the Earth's core through a process known as planetary differentiation. Early in Earth's formation, heavy elements like iron and nickel sank toward the center due to gravitational forces, while lighter elements, such as oxygen and silicon, remained in the mantle and crust. This process was facilitated by the intense heat from radioactive decay and the energy from collisions with other celestial bodies, causing the molten materials to separate based on density. Over time, this led to the formation of distinct layers, with the heaviest elements concentrated in the core.

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1mo ago

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