The pressure of the Earth's continental crust varies with depth, typically increasing with the weight of overlying material. On average, the pressure increases by about 25-30 megapascals (MPa) for every kilometer of depth. At the crust's average thickness of about 30 kilometers, the pressure can reach around 750-900 MPa. This pressure is significant enough to influence geological processes, including rock formation and metamorphism.
continental crust
it has been washed into the oceans as the continental crust has eroded.
The largest layer of Earth's surface is the crust, which is divided into oceanic and continental crust. The continental crust is thicker and less dense than the oceanic crust, covering about 40% of the Earth's surface.
Oceanic crust is denser than continental crust. Oceanic crust has a density of about 3 g/cm^3, while continental crust has a lower density of about 2.7 g/cm^3.
Earths crust can break under pressure and milk can break its foundation from pressure, both are different types of pressure, but still
continental crust
continental crust
Water
The continental crust is about 25 to 70 kilometers thick. The average is about 50 kilometers.
well, to be technical the earths crust is really on the inner outside
Continental plates.
Carbon
Oceanic
it has been washed into the oceans as the continental crust has eroded.
Earth's oceanic crust is thinner, denser, and younger than Earth's continental crust. It is primarily composed of basaltic rock, whereas continental crust is made up of less dense granitic rock. Oceanic crust is constantly being formed at mid-ocean ridges and destroyed at subduction zones.
Plate tectonic movement and subduction zones.
oceanic crust is made of basalt while continental crust is made of silica rich rocks like granite.