the lithosphere is thinner under the oceanic crust
The two layers of the lithosphere is made up of the oceanic lithosphere and continental lithosphere. The oceanic lithosphere is associated with oceanic crust and the ocean basins. The continental lithosphere is associated with the continental crust.
Oceanic crust is thinner and denser than continental crust.
Oceanic crust is thinner and of greater density than continental crust.
The density of the continental (granitic) lithosphere is lower than oceanic (basaltic) lithosphere. Consequently, due to buoyancy, the continental crust rides above the oceanic lithosphere and thus is not subducted. However, it is thought that pieces of the continental lithosphere break off and are subducted along with the oceanic lithosphere.
There are two types of crust, there is the oceanic and the continental crust.
It is not. The oceanic crust is thinner than the continental crust!
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.
The two layers of the lithosphere is made up of the oceanic lithosphere and continental lithosphere. The oceanic lithosphere is associated with oceanic crust and the ocean basins. The continental lithosphere is associated with the continental crust.
Oceanic crust is thinner and denser than continental crust.
It is not. The oceanic crust is thinner than the continental crust!
Continental
Continental lithosphere is thicker and less dense than oceanic lithosphere. Continental crust is primarily composed of granitic rock while oceanic crust is composed primarily of basaltic rock.
Oceanic crust is thinner and of greater density than continental crust.
Continental crust is thicker but less dense, and oceanic crust is thinner but more dense, making it heavier.
In general the Earth's oceanic crust is thinner then the continental crust
The density of the continental (granitic) lithosphere is lower than oceanic (basaltic) lithosphere. Consequently, due to buoyancy, the continental crust rides above the oceanic lithosphere and thus is not subducted. However, it is thought that pieces of the continental lithosphere break off and are subducted along with the oceanic lithosphere.
There are two types of crust, there is the oceanic and the continental crust.