Describe the interior of the earth
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Explanation:
interior Structure of earth’s interior is fundamentally divided into three layers – crust, mantle and core
Crust
- It is the outermost solid part of the earth, normally about 8-40 kms thick.
- It is brittle in nature.
- Nearly 1% of the earth’s volume and 0.5% of earth’s mass are made of the crust.
- The thickness of the crust under the oceanic and continental areas are different. Oceanic crust is thinner (about 5kms) as compared to the continental crust (about 30kms).
- Major constituent elements of crust are Silica (Si) and Aluminium (Al) and thus, it is often termed as SIAL
Mantle
- the portion of the interior beyond the crust is called the mantle.
- It is in a solid-state.
- It has a density higher than the crust portion.
- The thickness ranges from 10-200 km.
- The crust and the uppermost part of the mantle are called the lithosphere.
- The major constituent elements of the mantle are Silicon and Magnesium and hence it is also termed as SIMA
Core
- The core-mantle boundary is positioned at the depth of 2,900 km.
- The inner core is in the solid-state whereas the outer core is in the liquid state.
- The core is made up of very heavy material mostly constituted by nickel and iron. Hence it is also called the “nife” layer.
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