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Q: How does the oceanic plate move?
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Related questions

Do continental plates move faster than oceanic plates?

No, oceanic plates move faster than continental plates. This is due to the density of the oceanic plates (basalt is denser). For example, the fastest moving plates are the Pacific plate, Cocos plate, and Nazca plate. All oceanic.


Why do oceanic plates move under continental plates when the two collide?

Oceanic plates move under continental plates when they converge together because the oceanic plate is more denser than the continental plate.


Is the Pacific plate and oceanic plate or continental plate?

It is oceanic


Is the antarctic plate an oceanic or continental plate?

The Antarctic plate is Oceanic.


Is the arabian plate continental or oceanic?

oceanic plate


When a continental crustal plate collides with an oceanic crustal plate the continental crust is forced to move over the oceanic crust What is the primary reason that the continental crust stays on?

Continental crust is less dense than oceanic crust.


What happens to an oceanic plate as it pushes against a continental plate and sinks?

The oceanic plate sinks into the mantle where it melts. This is replaced by new oceanic plate at the mid-oceanic ridge.


What forms where an oceanic plate begins to move down in a subduction zone?

Convergent Boundaries


What forms where a oceanic plate begins to move down in a subduction zone?

Convergent Boundaries


When a continental plate and an oceanic plate collide why does the oceanic plate sink below the continental plate?

It's because the oceanic plate is more dense than the continental plate.


What are the differences between the three types of plate boundaries?

divergent, transform and convergent divergent plate boundaries move away from each other, convergent plate boundaries move toward each other, and transform plate bounties slide past each other.


Why does the oceanic crust move below continental crust?

The basaltic oceanic crust is more dense than the granitic continental crust. Therefore, when the two meet at plate margins, the oceanic crust usually subducts beneath the continental plate.