As a whole, on the basis of seismic investigations, the earth’s interior has been broadly divided into three major parts:
1. The Crust
2. The Mantle
3. The Core
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(a) the crust, mantle and core are separated by two sharp breaks, usually known as major discontinuities;
(b) the crust is having an average thickness of about 33 kms;
(c) the crust is composed of heterogeenous materials;
(d) the second major segment of the earth, i.e the mantle extends from below the crust to a depth of 2900 kms;
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(e) the third major segment of the earth i.e. the core extends from below the mantle upto the centre of the earth;