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The density and thickness of the earth crust varies depending on if you are looking at oceanic or continental crust. The oceanic crust's density averages to around 2900 kg/m3 and ranges from 7 to 10 kilometers thick. The continental crust's density averages to around 2700 kg/m3 and ranges 25 to 70 kilometers thick.
volume = mass . density v = 3.6 v = lbh h = (lb)/v h = 36.4
No. Controlled burning is actually necessary to decrease it's density.
It remains the same.
Along their colliding (convergent) boundary.
thickness
Crustal rock is normally less dense than mantle rock.
yes
density
Density
Volume= Length x Height x thickness = Mass ---------- Density So, Thickness = Mass ---------------------------------- Density x Length x Height
If the density AND the diameter are the same, then the coin with double thickness has double the mass.
It Depends on its thickness
The center of gravity of a triangle can be found by adjusting the thickness. You also need to find the density at the intersection.
The crustal plates (made mostly of low density granitic rock) float on the mantle (made mostly of high density basaltic rock). Convection cells in the mantle move the floating crustal plates around.
falseThe Earth's crust is quite variable in density and thickness. Some places on the ocean floors it is many miles thinner than on land.
The answer depends on what characteristic you wish to measure: its length, width, thickness, density, rigidity, etc.The answer depends on what characteristic you wish to measure: its length, width, thickness, density, rigidity, etc.The answer depends on what characteristic you wish to measure: its length, width, thickness, density, rigidity, etc.The answer depends on what characteristic you wish to measure: its length, width, thickness, density, rigidity, etc.