The Mid-Atlantic Ridge is a classic example of an oceanic divergent plate boundary.
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
The landforms that could develop at a continental and oceanic divergent plate boundary includes; Rifts and Volcanic Mountains.
none
continetal and oceanic
The Mid-Atlantic Ridge is a classic example of an oceanic divergent plate boundary.
divergent boundaries
New oceanic crust is created at the mid-oceanic ridges, a divergent plate boundary.
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
rift
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The landforms that could develop at a continental and oceanic divergent plate boundary includes; Rifts and Volcanic Mountains.
Yes; at divergent/constructive boundaries, plates move apart and new oceanic lithosphere forms.
On the seafloor. Yes, the mid oceanic ridges are all divergent boundaries.
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 volcanic landforms at divergent ocean plate boundaries are oceanic ridges.
continetal and oceanic