Density will vary from place to place with ocean crust being denser than continental crust.
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.
crust
The density of oceanic crust is generally higher than continental crust due to its composition of mostly basaltic rock. This higher density causes oceanic crust to be thinner and denser, leading to its subduction beneath continental crust at convergent plate boundaries.
it is 3.0 g.\cm to the third power. Your welcome.
Another word for Earth's outer surface is "crust."
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 lithosphere and the crust of the earth are the same lithosphere is another word for crust so the thickest is both of them.
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 amount of crust present on Earth always stays the same. The amount of crust descending into the mantle is balanced by the amount of crust formed at mid-ocean ridges.
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