The Moho
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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.
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.
Oceanic crust and continental crust are the two types of crust involved at a convergent boundary where an oceanic plate subducts beneath a continental plate.
No, new crust is not created at a convergent boundary. Instead, at convergent boundaries, two tectonic plates come together and one plate is usually forced beneath the other in a process called subduction. This process can lead to the destruction of crust rather than the creation of new crust.
The boundary between the oceanic crust and continental crust is known as the continental shelf. This is the shallowest part of the ocean that extends from the shore to the continental slope.
Moho stands for Mohorovičić discontinuity, which is the boundary between the Earth's crust and mantle.