The Structure of the Earth-

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Planet Earth

The Structure of the Earth-

The Crust:         

This region is thin compared to the other layers in the Earth.  It varies in thickness from 10km deep to 65km deep.  The crust is made up of lighter rocks that "float" on top of the mantle.  This layer includes the continents as well as the rock under the oceans.  The thickness of the crust might be a little deceiving... to put it into perspective, we have built many deep mines but NONE have yet reached the mantle!

The Mantle:

This region lies under the crust and is approximately 2900km thick.  The mantle is much denser than the crust (which is why the crust floats on top) and has a texture much like tar.  The rock in this region is rich in compounds made from iron, magnesium, and silicon, which accounts for why it is denser than the crust.

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The Core:

This region is divided into two parts.  The outer part is called the Outer Core.  It is about 2100km thick and made of liquid nickel and iron.  The inner part is called the Inner Core and it is the real centre of the Earth.  This part is about 2800km in diameter and is made of solid iron and nickel.

Plate tectonics

Plate tectonics are a reasonably new theory that has revolutionized the way geologists thinks about the Earth. According to the theory, the surface of the Earth is broken into large plates. The size and position ...

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