The Mohorovičić discontinuity (the Moho) separates the mantle and the crust.
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The Moho separates the crust and the mantle.
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).
The Moho separates the crust and the mantle.
No, instead of another crust, the sometimes magnesium rich Mohorovičić discontinuity separates the crust from the iron rich mantle.
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.
It is composed of very hot rock that is "plastic" (slowly moving and deforming). It is not as liquid as the outer core, or the magma that separates the crust from the mantle.
The Mohorovičić discontinuity (Moho) separates the Earth's crust from the underlying mantle. It is found beneath continents and beneath ocean basins.
The Moho, short for Mohorovičić discontinuity, is a boundary in the Earth's crust that separates the solid crust from the underlying mantle. So, the Moho is where the solid crust transitions into the solid mantle, but it is not a solid or liquid layer itself.
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).
Mohorovicic discontinuity is located between the upper mantle and the crust, while the Gutenberg discontinuityis located between the lower mantle and the outer core.
The upper mantle and the lower mantle.
The Moho Barrier is characterized by a seismic velocity discontinuity that separates the Earth's crust from the underlying mantle. It is located at an average depth of about 25-35 kilometers beneath continental crust and 5-10 kilometers beneath oceanic crust.