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Earth differentiated due to the intense heat generated from the decay of radioactive elements, the impact of planetesimals during its formation, and the gravitational compression of materials. This process caused denser materials, like iron and nickel, to sink toward the center, forming the core, while lighter materials, such as silicates, rose to create the mantle and crust. As a result, Earth developed distinct layers with varying compositions and properties, leading to the formation of a stable, geologically active planet capable of supporting life.

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