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Oceanic crust is thinner and more dense will continental crust is thicker and less dense.
There are two types of lithosphere: the oceanic lithosphere and the continental lithosphere. The oceanic lithosphere exists in the ocean basins while the continental lithosphere exists in the continental crust.
Oceanic crust is more dense than continental crust.
The Earth's crust includes oceanic and continental categories, the oceanic crust composed of basalt rock and recycled in roughly 150 million year intervals by lithospheric plate movements, and the older less dense continental crust, composed of granitic rock.
The crust and upper mantle
Oceanic crust is thinner and more dense will continental crust is thicker and less dense.
There are two types of lithosphere: the oceanic lithosphere and the continental lithosphere. The oceanic lithosphere exists in the ocean basins while the continental lithosphere exists in the continental crust.
Tectonic plates are also "Continental Crust" and "Oceanic Crust". Also lithospheric plates.
Typically the less dense continental plate would stay afloat while the denser oceanic plate would be submerged below. This can result in volcanic eruptions at the subduction zone due to oceanic crust undergoing increased pressure and temperatures as it descends below the continental crust.
It is possible to have continental and oceanic crust on the same plate. The only to this exception is with the Pacific plate which exists independently.
Oceanic crust is more dense than continental crust.
The Earth's crust includes oceanic and continental categories, the oceanic crust composed of basalt rock and recycled in roughly 150 million year intervals by lithospheric plate movements, and the older less dense continental crust, composed of granitic rock.
Continental crust A+
what is the continental crust
Soil is the topmost layer of the Earth's crust.
The crust and upper mantle
continental crust