Crust: The outer most layer or shell of the earth is known as earth’s crust. On an average it is
30km deep. It can be up to 70km under high mountains and up to 8km under ocean. It
represents less than 1% of earth’s total volume and its average density is 2.7 gm/cm3. It is
known as ‘sial’ because of abundance of silicon and aluminium. It is also divided into upper and
lower crust divided by Connarddiscontinuity.a
Mantle: The second layer of earth is called mantle. It is separated from crust by Mohorovicic
discontinuity. Its density ranges from 3.3 to 5.7. It is made of dense and rigid rocks which have
the predominance of magnesium and silicon, known as ‘sima’. It is also separated
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