We can’t get direct information about the interior of the earth.
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Earth's interior is generally divided into three major layers: the crust, the mantle, and the core. The hard, brittle crust extends from Earth's surface to the so-called Mohorovicic discontinuity, nicknamed the Moho. ... Beneath the Moho is the mantle, the viscous layer that makes up more than half of Earth's volume.
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We can’t get direct information about the interior of the earth because the pressure and temperature of the earth’s interior is very high
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