The average density of the Earth's crust is 2.7 grams per cubic centimeter.
POP DENSITY
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.
Because the density of the force increases.
The Earth's crust is the thinnest layer, ranging from about 5-70 km thick. The average density of the Earth's crust is around 2.7-3.0 g/cm³.
subduction is when a piece of the earths crust slides back into the mantle due to density differences
The Earth's compositional layers in order of increasing density are the crust, mantle, outer core, and inner core. The crust is the least dense layer, while the inner core is the most dense layer.
The Earths crust is approximately 650 km deep.
The layers of Earth's interior from least to greatest density are: Crust Mantle Outer core Inner core
The sudden vibration in the plates inside the crust causes the earths crust to rise & fall.
mantle
The earth's crust is not stress
half of earths layer