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Properties and Composition of the Earth's Crust. The continental crust is between 10 km and 70 km thick, depending on the location. As you descend through the crust, the temperature increases from surface temperature to between 300 degrees Celsius and 500 degrees Celsius.ontinental crust is between 10 km and 70 km thick, reaches temperatures as high as 500 degrees Celsius, pressures as high as 91,000 atmospheres, and is made up of rock that is mostly felsic and granitic. It is thanks to the formation of continental crust that humans and all land-evolved species exist.
Accordingly, the crust is divided into two types; the continental crust and the oceanic crust. Oceanic Crust. The oceanic crust is that part of the Earthâs crust that covers the ocean basins. It consists of dark-colored rocks made up of basalt.This rock is made up of silicon, oxygen, and magnesium.The density of the oceanic crust is about 3.0 g/cm3.The continental crust has a lower density. This difference in the average densities allows many natural phenomenon to occur on and below the surface of the Earth. The oceanic crust scarcely floats on the mantle.t consists of dark-colored rocks made up of basalt. This rock is made up of silicon, oxygen, and magnesium. The density of the oceanic crust is about 3.0 g/cm3. The continental crust has a lower density.