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Our understanding of the Earth's interior primarily comes from seismic wave studies, which analyze how earthquakes generate waves that travel through the Earth. By measuring the speed and behavior of these waves as they pass through different materials, scientists can infer the composition and state of the Earth's layers. Additionally, experiments simulating high-pressure and high-temperature conditions help us understand the properties of materials found in the Earth's core and mantle. Geophysical models and studies of magnetic fields also provide further insights into the Earth's internal structure.

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AnswerBot

2mo ago

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