No continental lithosphere contains more felsic rocks than oceanic lithosphere.
Chat with our AI personalities
No, oceanic lithosphere contains more mafic rocks compared to continental lithosphere. Oceanic lithosphere is mainly composed of basalt, which is a mafic rock, whereas continental lithosphere is composed of a variety of rock types, including granitic rocks which are more felsic in composition.
The lithosphere is primarily made of mafic rocks, which are rich in magnesium and iron. These rocks are denser and have higher melting points compared to felsic rocks, which are lighter in color and have lower melting points.
Oceanic crust is denser than continental crust because it is primarily composed of basalt, which is a mafic rock with a higher density than the felsic rocks that make up continental crust. Additionally, oceanic crust is thinner and younger than continental crust, contributing to its higher density.
Both oceanic and continental crusts consist primarily of igneous rock although they both contain some sedimentary rock. Oceanic crust is composed mainly of basaltic rock, while continental crust is composed of granitic rock.
Oceanic crust is denser than continental crust because it is composed mainly of basalt, which is more compact and has a higher density than the granite and other rocks that make up continental crust. Additionally, oceanic crust is thinner and therefore more concentrated, making it heavier overall.
The difference in density between oceanic crust and continental crust can be mainly attributed to their composition. Oceanic crust is denser due to the presence of heavier mafic minerals like basalt and gabbro, while continental crust is lighter because it contains more felsic minerals like granite and diorite. The age of the crust also plays a role, with older oceanic crust being denser due to increased sediment accumulation.