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.
The portion of the continental margin that serves as a boundary between the oceanic crust and the continental crust is known as the continental slope. This region transitions from the relatively shallow continental shelf to the steeper continental rise, leading down to the deep ocean floor. The slope marks the edge of the continental crust, where it meets the denser oceanic crust beneath the ocean.
Convergent boundary.
Convergent boundary.
Divergent Boundary, (Constructive Boundary).
New crust is being added to the other edge of the boundary
the continental shelf, which is an underwater landmass extending from the shoreline to the continental slope. This boundary represents the transition from continental crust to oceanic crust and generally marks the end of the continent.
No. New oceanic crust is formed at a divergent boundary. A convergent boundary neither creates nor destroys crust.
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 plate boundary.
Convergent boundary.
Divergent Boundary, (Constructive Boundary).
This would be called a Spreading center, or a divergent plate boundary.
Crust is formed at the edge of a tectonic plate by, when a volcano erupts, the lava or magma (same thing) hits the edge of a tectonic plate and cools and dries on the edge of that tectonic plate.
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.