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explanation of the internal structure of the earth in term of pressure​

Sagot :

itzNadeem

Explanation:

The pressure at the bottom of the mantle is ≈140 GPa (1.4 Matm). The mantle is composed of silicate rocks richer in iron and magnesium than the overlying crust. Although solid, the mantle's extremely hot silicate material can flow over very long timescales

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