Oceanic crust is both denser (and therefore heavier) and younger than continental crust.
The heavier (usually older and cooler hence more dense) oceanic crust normally subducts (is forced under) the younger less dense crust.
younger
Earth accreted from solid, heavier matter.
When comparing an oceanic crust and a landform crust, the oceanic crust will be much younger. Typically, an oceanic crust is less than 200 million years old.
They are two different types of crust. Continental crust is heavier than Oceanic crust, so when the two collide, the Continental crust 'subducts' under the Oceanic Crust. 'Crust' referring to the tectonic plates, the surface of the Earth we stand on.
The heavier (usually older and cooler hence more dense) oceanic crust normally subducts (is forced under) the younger less dense crust.
Trench
younger
younger
Oceanic crust is mafic in composition and continental crust is felsic in composition. Mafic minerals generally have a higher density than felsic minerals and therefore, the oceanic crust is heavier.
Continental crust is thicker but less dense, and oceanic crust is thinner but more dense, making it heavier.
Earth accreted from solid, heavier matter.
Oceanic crust is generally much younger. New ocean crust is constantly being formed.
When comparing an oceanic crust and a landform crust, the oceanic crust will be much younger. Typically, an oceanic crust is less than 200 million years old.
They are two different types of crust. Continental crust is heavier than Oceanic crust, so when the two collide, the Continental crust 'subducts' under the Oceanic Crust. 'Crust' referring to the tectonic plates, the surface of the Earth we stand on.
Ozone is away from crust. It founds suitable conditions for formation there.
The oceanic is heavier