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Granite and comparable rocks, often known as granitoids, dominate the continental crust. The chemical abundance and the rate of cooling of magma sometimes varieties a sequence often known as Bowen’s response series. Volcanic or extrusive rocks result from magma reaching the surface either as lava or fragmental ejecta, forming minerals such as pumice or basalt. Plutonic or intrusive rocks end result when magma cools and crystallizes slowly inside the Earth’s crust. Most rocks contain silicate minerals, compounds that include silicon oxide tetrahedra in their crystal lattice, and account for about one-third of all recognized mineral species and about 95% of the earth’s crust.
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