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The layers of the Earth can be divided into layers according to its chemical composition as we can see in the picture. These layers are called... | Crust Mantle Outer core Inner core |
The crust is made up of...
Image:
Crust (binary/octet-stream)
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less dense rocks, rich in silicon and aluminium |
The mantle is composed of...
Image:
Mantle (binary/octet-stream)
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denser rocks like magnesium |
The core is principally made up of...
Image:
Core (binary/octet-stream)
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iron and other metals. |
These are the three discontinuity boundaries: Mohorovicic discontinuity Gutenberg discontinuity Lehmann discontinuity | |
The Mohorovicic discontinuity marks the boundary between | the crust and the mantle |
The Gutenberg discontinuity marks the boundary between | the mantle and the outer core |
THe Lehman discontinuity marks the boundary between | the outer core and the inner core |
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