The asthenosphere is in a semi-molten state
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The temperature and pressure of the asthenosphereare so high that rocks soften and partly melt, becoming semi-molten. The asthenosphere is much more ductile than either the lithosphere or lower mantle.
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At the Depth of 100-250km the mantle is partially molten and known as asthenosphere due to temperature 1100 degree Celsius along with greater density and pressure.
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