Scientists have determined the composition of Earth's layers primarily through seismic studies, which analyze how seismic waves generated by earthquakes travel through the Earth. By studying the speed and behavior of these waves as they pass through different materials, researchers can infer the density and composition of various layers. Additionally, samples from volcanic eruptions and deep drilling projects provide direct evidence of the materials present in the Earth's crust and upper mantle. Laboratory experiments simulating high-pressure conditions also help scientists understand how materials behave under the extreme conditions found in the Earth's interior.
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