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The mantle, situated between the Earth's crust and core, accounts for about 84% of the Earth's total volume, making it the most voluminous of the three major concentric zones. It is composed primarily of silicate minerals and is characterized by a semi-solid state that allows for slow, convective movements. These movements play a crucial role in plate tectonics and the recycling of materials within the Earth. The mantle's dynamics significantly influence geological processes, including volcanic activity and the formation of mountain ranges.

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2mo ago

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