less dense and more felsic
thinner and denser
The continental shelf is normally made out of continental crust, the oceanic crust begins at the base of the continental rise. However in most places the oceanic crust near the continental margins is covered by continental sediments (eroded form the continents) carried down onto the Oceanic planes by deep sea canyons running off the continental rises.
Oceanic crust is thinner and denser than continental crust.
Continental crust.
Thickness - continental = much thickerDensity - oceanic crust is denser than continental, which is why the oceanic crust subducts under the continental at destructive plates boundaries.
thinner and denser
Iron and magnesium, when compared to continental crust.
thinner and denser
The composition of the continental crust is granitic overall, high in silicon and aluminum, when compared to the oceanic crust.
The continental shelf is normally made out of continental crust, the oceanic crust begins at the base of the continental rise. However in most places the oceanic crust near the continental margins is covered by continental sediments (eroded form the continents) carried down onto the Oceanic planes by deep sea canyons running off the continental rises.
No, the oceanic crust is denser. That's why the land areas "float" so much higher than the ocean bedrock.
It is not. The oceanic crust is thinner than the continental crust!
Oceanic crust is thinner and denser than continental crust.
Continental crust is far older than oceanic crust.
Continental crust.
Thickness - continental = much thickerDensity - oceanic crust is denser than continental, which is why the oceanic crust subducts under the continental at destructive plates boundaries.
The Oceanic crust is denser than the continental crust