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The asthenosphere is a semi-fluid layer of the Earth's mantle located beneath the lithosphere, extending from about 100 to 700 kilometers below the surface. It is characterized by its ability to flow slowly over geological time due to high temperatures and pressures, which allow rocks to behave like a viscous fluid. This layer plays a crucial role in tectonic plate movements, as it provides a lubricating layer that enables the rigid lithospheric plates to glide over it. The asthenosphere is also less rigid than the overlying lithosphere, with lower seismic wave velocities indicating its partially molten state.

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2w ago

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