The Mohorovičić discontinuity (the Moho) separates the mantle and the crust.
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The Mohorovicic Discontinuity (also known as the Moho) separates the Earth's crust from the underlying mantle. It is the boundary where seismic waves change speed, indicating a change in composition and density between the two layers.
The Mohorovicic Discontinuity, generally referred to as the Moho, where seismic waves increase in velocity.
There is a separation between the mantle and crust of the earth. A seismic discontinuity called the Mohorovicic discontinuity forms that boundary.
The Moho discontinuity separates the Earth's crust from the underlying mantle. This boundary is located between the crust and the uppermost part of the mantle known as the lithosphere.
The boundary that separates the Earth's crust and the cooler part of the mantle is called the Mohorovičić discontinuity or Moho. It marks the transition between the Earth's crust and the uppermost part of the mantle.
The mantle is located directly beneath the Earth's crust and is approximately 1,800 miles (2,900 kilometers) thick. The boundary between the crust and the mantle is known as the Mohorovičić discontinuity or Moho.
It is between the Crust and the upper mantle
The Moho boundary separates the Earth's crust from the mantle. It marks the boundary between the Earth's rigid outer layer (crust) and the underlying, more ductile layer (mantle).