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The two primary layers of the Earth are the crust and the mantle. The crust is the thin, outermost layer where we live, while the mantle lies beneath it and extends to a depth of about 2,900 kilometers (1,800 miles). The mantle is composed of semi-solid rock and plays a crucial role in tectonic activity. Additionally, beneath the mantle is the outer core and the inner core, which are also significant layers of the Earth's structure.

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