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continental is more buoyant
Oceanic crust is significantly denser.
The continental crust is less dense than the oceanic crust. That's the reason we find that the oceanic crust sinks (subducts) beneath the continental crust.Continental crust is less dense than oceanic crust and so cannot sink below it.
This is because the Oceanic Crust is denser and thinner than the Continental Crust and is actively being created by the forces of the magma at different mid-oceanic ridges.
The Oceanic plate is subducted under the Continental plate because oceanic crust is much more dense than continental crust. The average density of the oceanic crust is 3g/cm^3 while the average density of continental crust is 2.7g/cm^3.
continental is more buoyant
Continental plates are more buoyant then oceanic plates.
This is because the land mass is more buoyant, or lighter, than the oceanfloor.
Continental lithospheric plates are more buoyant than oceanic plates, yes.
Continental crust.
Oceanic crust is more dense than continental crust.
oceanic crust is much more dense than continental crust. Oceanic crust is also responsible for the movement of continental crust.
There are two types of crust, and they are the oceanic crust and the continental crust. Oceanic crust is thinner yet more dense than continental crust, and continental crust is on average older than oceanic crust :)
False! When two continental plates converge a mountain range is formed. This is what formed and is continuing to "build" the Himalayan mountain chain.Subduction zones form where oceanic crust converges with and is forced under continental crust, or younger more buoyant oceanic crust.
The continental crust is the land. The oceanic is under the ocean.
Continental crust is thicker but less dense, and oceanic crust is thinner but more dense, making it heavier.
Two differences are that the oceanic crust is more dense than continental, and continental crust is composed mostly of granite, while oceanic is mostly basalt