The Moho
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.
The two types of Crust is the Continental Crust and the Oceanic Crust.
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.
Another name for a constructive boundary is a divergent boundary. This type of boundary occurs when two tectonic plates move away from each other, leading to the formation of new crust. It is characterized by volcanic activity and the creation of rift valleys.
New crust is being added to the other edge of the boundary
No. New oceanic crust is formed at a divergent boundary. A convergent boundary neither creates nor destroys crust.
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.
Convergent boundary.
Divergent plate boundary.
Convergent boundary.
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.
Divergent Boundary, (Constructive Boundary).
This would be called a Spreading center, or a divergent plate boundary.
Constructive because new land is 'constructed'
transform boundary
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.