Layers of the Earth
Layers of the Earth
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Earth layers. NASA. Wikipedia. (Public Domain) |
The Geosphere is the solid part of the Earth consisting of several layers: crust, mantle, outer core and inner core. |
Crust: It is the outermost layer of the Earth. It's made of solid rocks, mainly granite and basalt, and minerals. It is 40 km deep and it is divided into oceanic crust and continental crust. |
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Mantle: It is the second layer of the Earth. It is about 2,900 km deep and has two parts: - the upper mantle, which contains solid and molten rocks. - the lower mantle, which mainly contains solid materials. |
Oceanic-Continental convergence. William Crochot. Wikipedia. (Public Domain) |
Crust
Mantle
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| Outer core: It is such a hot layer that metal and rocks get melted so it is a molten layer. It contains mainly iron but also nickel, oxygen and sulfur. It is about 2,400 km deep. | Inner core: It is the hottest layer and the centre of the Earth. It is solid because there is a lot of pressure in it. It is mainly made up of an iron-nickel alloy but there are also other metals. It is about 1,200 km deep. |
Outer core
Inner core
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Activity 1
Activity 2
Activity 3
Extra activity
Inge Lehmann
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