Convergent
The mid-ocean ridge system is the longest continuous divergent plate boundary on Earth.
o mid ocean ridge
A mid ocean ridge is a diverging plate boundary so the simple answer is yes.
A divergent plate boundary
at the mid-ocean ridge you can find the youngest oceanic plate and a divergent boundary.
The Mid-Atlantic Ridge separates the North American plate from the African plate. This ridge runs through the Atlantic Ocean and marks the boundary where the two plates are moving apart.
A mid-ocean ridge forms at the divergent plate boundary. This boundary initially forms rifts that later on become rift valleys.
The mid-ocean ridge is formed along a divergent or constructive plate boundary between two plates of oceanic crust. A classic example is the Mid-Atlantic Ridge where the Eurasian and African Plates are moving away from the North and South American Plates.
A divergent plate boundary creates a mid-ocean ridge. This occurs when two tectonic plates move away from each other, leading to the upwelling of magma from the mantle, creating new oceanic crust at the mid-ocean ridge.
The mid-ocean ridge is a divergent plate boundary where tectonic plates are moving away from each other. As the plates separate, magma rises to the surface, creating new oceanic crust.
A mid-ocean ridge forms at the divergent plate boundary. This boundary initially forms rifts that later on become rift valleys.
The mid-ocean ridge is formed along a divergent or constructive plate boundary between two plates of oceanic crust.