the discontinuity between Crust and Mantle
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The Mohorovicic Discontinuity, or "Moho," is the boundary between the crust and the mantle. The red line in the diagram shows its location. In geology the word "discontinuity" is used for a surface at which seismic waves change velocity.
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The top layer of earth is called crust.
the middle layer is called as mantle
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