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The boundaries that separate the layers of the Earth's interior are called "discontinuities." The most notable of these include the Mohorovičić discontinuity (Moho), which separates the crust from the mantle, and the Lithosphere-Asthenosphere boundary, which separates the rigid lithosphere from the more ductile asthenosphere beneath it. Other significant discontinuities exist between different layers of the mantle and between the mantle and the outer core.

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