why is the composition of the srystal layer of the earth of great interest
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The internal structure of the Earth is layered in spherical shells: an outer silicate solid crust, a highly viscous asthenosphere and mantle, a liquid outer core that is much less viscous than the mantle, and a solid inner core. The force exerted by Earth's gravity can be used to calculate its mass.
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The internal structure of the Earth is layered in spherical shells: an outer silicate solid crust, a highly viscous asthenosphere and mantle, a liquid outer core that is much less viscous than the mantle, and a solid inner core. The force exerted by Earth's gravity can be used to calculate its mass.
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