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igneous rock formed by cooling and crystallization of magma at the earth's surface |
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igneous rock formed by cooling and crystallization of magma at great depth beneath the earth's surface |
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classification of the igneous rocks |
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based on chemical and mineral composition, grain size |
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controlled by rate of cooling of the magma, and viscosity of the magma |
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cooling is too rapid for ions to group into crystals |
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glass of felsic composition |
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an igneous rock in which large crystals are enclosed in a matrix of much finer grained minerals |
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biotite, amphibole, pyroxene, olivine |
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distribution of igneous rocks in the earth's crust |
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-rock formed from magma of granitic composition is confined to the continental crust |
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