INTERIOR OF THE EARTH can be discussed in THREE LAYERS-
1. CRUST
2. MANTLE &
3. CORE
It is the outermost solid part of the Earth. It is brittle in nature. Because, during an earthquake, it is the crust that breaks easily. causing a FAULT. The more and more the density of material increases as we go more and more deep. So, materials available in the crust level have low density. The thickness of the crust varies under the Oceanic and the Continental areas.
The mean thickness of OCEANIC CRUST is 5 km.
Whereas the CONTINENTAL CRUST is around 30 km.
The second layer is the mantle. Right from the end of the crust and the beginning of outer core it is 2900 km deep and divided into TWO parts-
Upper mantle- it is also called ASTHENOSPHERE and upper mantle and crust together called the LITHOSPHERE. Astheno means weak and due to this weakness the magma finds way to the surface during volcanic eruption. Thickness of the lithosphere is 200 km.
Lower mantle- This layer is also responsible for all of earth's volcanic and seismic activity. Because 2900 km thickness is pretty specious area for the formation of such natural catastrophe. Because, after some laboratory tests it has found that temperature under 100-200 km of earth surface is very high that the rocks are in Molten State.
It is the immediate next layer of the Mantle part of the earth. Density of the materials in this layer is 3500 km. And divided into TWO parts-
OUTER Core- This part is generally in liquid state. The depth is 2300 km and consists of Ni (nickel) and Fe (iron). Because of these two chemical constituents this layer is also known as Nife layer. The highest temperature in this layer is around 4000-5000 degrees Celsius.
INNER Core- This part is generally in solid state. The depth is 1200 km and consists of Fe (iron) mainly. The temperature goes to 5000-7000 degrees Celsius.
