Explain the interior of the Earth with the help of a diagram.
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>>Earth's interior is made up of a series of layers that sit below the surface crust. In order of depth, these layers include the solid, but flowing mantle, the liquid outer core and the solid iron outer core, which helps create Earth's protective magnetic field.
>>Most of what we know about the interior of the Earth comes from the study of seismic waves from earthquakes. ... These waves contain vital information about the internal structure of the Earth. As seismic waves pass through the Earth, they are refracted, or bent, like rays of light bend when they pass though a glass prism.
>>Earth scientists inherited a rather simple picture of Earth's interior from their pre-plate tectonics colleagues. ... Seismic waves passing through the deep Earth suggested that beneath the broken skin of plates lies a 2800-kilometer layer of rocky mantle overlying 3470 kilometers of molten and—at the center—solid iron
>>See the attachment for diagram✌
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Explanation:
The above diagrams are the cross sections of the earth.
In order to see temperature increases of about 25°C per kilometre, we only need to drill a short distance. As a result, everything may eventually become so hot that we will run into molten rock, similar to the lava that flows from volcanoes.
Common sense, however, tells us that this quick increase in temperature that surface drilling has revealed could not last forever since then the Earth's core would be hotter than the Sun.
According to the widely recognised idea of the Earth's structure, the planet is made up of a silicate crust, a viscous mantle, and solid inner and liquid outer cores.
We think that melting and gravitational attraction have finely sorted the Earth's makeup so that
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