Oceanic crust is the part of Earth's lithosphere that surfaces in the ocean basins.
Oceanic crust is primarily composed of mafic rocks, or sima, which is rich in iron and magnesium.
It is thinner than continental crust, or sial, generally less than 10 kilometers thick, however it is denser, having a mean density of about 2.9 grams per cubic centimeter.[1]
As oceanic plates slide away from each other, magma rises. It come to the ocean floor and starts to cool. Then after years and years it starts to build up on this creating oceanic plates.
there is no lasgical answer
The oceanic plates are mostly made up of Basalt
Primarily of basalt, with a crust of sediment or sedimentary rock.
Basalt. An igneous rock.
yes but oceanic crust is younger than continental crust because of deep sea trenches
Oceanic plates are young and made of basalt and recent sediments. Continental plates are old and contain continental crust made of old rocks and they are usually considerably thicker than the oceanic plates
plates There are continental plates (thick and made of granite) and oceanic plates (thin and made of basalt).
The two types of tectonic plates are continental and oceanic.
Continental plates are composed of mainly granitic rock.
The main mineral type in Oceanic plates are made of basalt
mostly made of basalt.
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how many tectonic plates are made of oceanic crust
Basalt.
manganese
silicon Dioxide-silica
Tectonic plates may be made of continental crust, oceanic crust, or both.
yes but oceanic crust is younger than continental crust because of deep sea trenches
There are currently 14 continental and oceanic plates that make up the earth's crust.
Oceanic plates are young and made of basalt and recent sediments. Continental plates are old and contain continental crust made of old rocks and they are usually considerably thicker than the oceanic plates
AnswerThe continental plates are made up of largely granitic rock, while the oceanic plates are largely basaltic rock. Certainly some other types of rock are included, but these are the largest contributors to the material or composition. A link is provided below for more information.