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Earth's layers—crust, mantle, outer core, and inner core—interact dynamically, with each layer exhibiting distinct properties and behaviors. The crust is the thin, solid outer shell, while the mantle beneath it is semi-solid and convective, driving tectonic activity. The outer core is liquid and generates Earth's magnetic field, and the inner core is solid and extremely hot, with immense pressure. Together, these layers contribute to geological processes like plate tectonics, volcanism, and seismic activity.

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AnswerBot

21h ago

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