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The Mid-Atlantic Ridge is a classic example of an oceanic divergent plate boundary.
The landforms that could develop at a continental and oceanic divergent plate boundary includes; Rifts and Volcanic Mountains.
The 3 general types are constructive, destructive, and conservative boundaries. Constructive (divergent) - plates move away from each other, typically creating a rift Destructive (convergent) - one plate will be subducted, or continental plates collide Conservative (transform) - plates grind past each other, stalling and slipping
No. New oceanic crust is formed at a divergent boundary. A convergent boundary neither creates nor destroys crust.
The magma flows upward from the split in the crust caused by the boundary.
An oceanic trench is formed. Divergent boundaries pull away from each other, forming a cavern in the ocean floor. The Marianas Trench is a good example of a divergent boundary.
The Mid-Atlantic Ridge is a classic example of an oceanic divergent plate boundary.
The landforms that could develop at a continental and oceanic divergent plate boundary includes; Rifts and Volcanic Mountains.
The 3 general types are constructive, destructive, and conservative boundaries. Constructive (divergent) - plates move away from each other, typically creating a rift Destructive (convergent) - one plate will be subducted, or continental plates collide Conservative (transform) - plates grind past each other, stalling and slipping
New oceanic crust is created at the mid-oceanic ridges, a divergent plate boundary.
rift
No. New oceanic crust is formed at a divergent boundary. A convergent boundary neither creates nor destroys crust.
Sea-Floor Spreading is your answer.
Oceanic - oceanic divergent boundary and Continental - oceanic divergent boundary.
The magma flows upward from the split in the crust caused by the boundary.
Divergent tectonic plate boundary
oceanic crest and volcano.