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The Moho

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11y ago
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5mo ago

The boundary at the bottom of the Earth's crust is called the Mohorovičić discontinuity, or more commonly, the Moho. It separates the crust from the underlying mantle based on differences in seismic wave velocities.

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Q: What is the name of the boundary at the bottom of the crust?
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Related questions

How can crust disappear at the edge of the boundary?

New crust is being added to the other edge of the boundary


Is a new oceanic crust formed at a transform fault boundary?

No. New oceanic crust is formed at a divergent boundary. A convergent boundary neither creates nor destroys crust.


How can crust disappear at the edge of a boundary?

Crust can disappear at the edge of a boundary through subduction, where one tectonic plate is pushed beneath another. This process causes the crust to be pulled into the mantle and reabsorbed, leading to the disappearance of crust at the boundary.


What type of boundary oceanic crust?

Convergent boundary.


What boundary does new crust form at?

Divergent plate boundary.


What type of boundary destroys oceanic crust?

Convergent boundary.


The boundary between continental crust and oceanic crust occurs at the base of the?

The boundary between continental crust and oceanic crust occurs at the base of the lithosphere. This boundary is known as the Mohorovičić discontinuity, or Moho. It separates the less dense continental crust from the more dense oceanic crust below.


What boundary is it called when new crust is being formed?

Divergent Boundary, (Constructive Boundary).


What type of boundary is new ocean crust crust formed?

This would be called a Spreading center, or a divergent plate boundary.


What type of boundary dose not create or destroy crust?

transform boundary


What is the name of the boundary were to plates of the earths crust move apart?

Constructive because new land is 'constructed'


Which plate boundary destroys crust?

Crust is destroyed at the convergent plate boundary. This is usually between the oceanic and continental plates. This is where subduction of the more dense crust occurs.