A tectonic boundary where two oceanic lithospheric plates are either moving away from one another and new crust is formed, or moving toward each other, in which the more dense oceanic plate will subduct beneath the less dense plate.
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An ocean-ocean plate boundary is a boundary where two oceanic plates move away from each other. This movement creates a mid-ocean ridge where new oceanic crust is formed through volcanic activity. In some cases, this boundary can also lead to the formation of island arcs through volcanic activity and subduction processes.
They are the same size
The mid-ocean ridge system is the longest continuous divergent plate boundary on Earth.
A mid ocean ridge is a diverging plate boundary so the simple answer is yes.
The plate boundary at which plates collide or come together is called a convergent boundary. At convergent boundaries, one plate is typically forced beneath the other in a process known as subduction. This collision can lead to the formation of mountain ranges, deep ocean trenches, and volcanic activity.
The Mid-Atlantic Ocean is a divergent plate boundary, where tectonic plates are moving away from each other. This movement creates new oceanic crust as magma rises from the mantle and solidifies at the mid-ocean ridge.