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ONLiNE UPSC
The Earth's mantle is the thickest layer of our planet, situated between the thin outer crust and the super-heated core.
It measures approximately 2,900 kilometers (1,800 miles) in thickness, comprising about 84% of the Earth's total volume.
The mantle is primarily composed of silicate rocks that are rich in elements like magnesium and iron. Although these rocks are mostly solid, they can flow very slowly over extended periods due to the intense heat and pressure present in this layer.
The mantle is divided into two main sections:
The mantle is crucial for many geological phenomena:
No, direct observation of the mantle is impossible due to its significant depth beneath the Earth's surface. However, scientists study the mantle indirectly through seismic waves, volcanic rocks, and laboratory experiments that simulate the conditions found within this layer.
Yes, scientists are continually researching the mantle to gain a deeper understanding of its composition, structure, and dynamics. These studies contribute to our knowledge of Earth's formation, evolution, and ongoing processes.
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