New crust is being added to the other edge of the 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.
No. New oceanic crust is formed at a divergent boundary. A convergent boundary neither creates nor destroys crust.
Convergent boundary.
A convergent plate boundary. a piece of continental crust and a piece of oceanic crust meeting at a convergent boundary.
The magma flows upward from the split in the crust caused by the boundary.
New crust is being added to the other edge of the boundary
No. New crust is created along a divergent boundary. Crust is destroyed at a convergent 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.
No. New oceanic crust is formed at a divergent boundary. A convergent boundary neither creates nor destroys crust.
Convergent boundary.
A convergent plate boundary. a piece of continental crust and a piece of oceanic crust meeting at a convergent boundary.
The magma flows upward from the split in the crust caused by the boundary.
Convergent boundary
Divergent plate boundary.
Convergent boundary.
The crust is part of the lithosphere, so there is no boundary between them. There is a boundary between the crust and the other part of the lithosphere which is the uppermost mantle. It is called the Mohorovicic Discontinuity or the 'Moho' for short.
Divergent Boundary, (Constructive Boundary).