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Molten rock that has not reached earths surface
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igneous rocks formed by subsurface cooling of magma. Coarse grain because slow rates of cooling
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igneous rocks formed from molten rock. Fast cooling fined grain
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process of rock melting in which minerals with low melting points melt before minerals with higher melting points as a rock mass is heated and/or subjected to a decrease in pressure
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concentration of crystals of particular mineral in portions of magma as it cools
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first crystals to form in a cooling magma settle to the bottom of magma chamber
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"mush" of precipitated crystals is separated from the magma by earths movements
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textural term; individual mineral crystals can be seen from unaided eye
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textural term; individual mineral crystals to small to see
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textural term; rapid cooling of lava gives glassy appearance
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large crystals enclosed by finer-grained matrix. Interrupted cooling history
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large crystals enclosed by finer-grained matrix. Interrupted cooling history
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large crystals enclosed by finer-grained matrix. Interrupted cooling history
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rock material ejected during volcanic eruption
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rock or minerals high in magnesium and iron and the magmas from which they form
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igneous rocks with high percentage of light colored minerals(quartz, feldspar, feldspathoids, muscorite)
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igneous rocks composed mostly of mafic minerals or magma from which they are formed
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ultramafic igneous rock, mostly olivine
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Dark colored, amorphous material, forms by superfast cooling
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Volcanic glass of various colors found in chilled margins of intrusive igneous bodies formed from basaltic magma
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coarse grain igneous rock, major component of continental crust
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less potassium feldspar than granite
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fined grain igneous rock; extrusive; found in andes mountains; 25-40% amphibole, pyroxime and biotite
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dark colored, fined grained, extrusive igneous rock; calcic plagioclase and pyroxenes
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coarse grain, ultramafic, plutonic, igenouse rock, composed mostly of olivine. Major component of upper mantle
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suite of rare igneous rocks noted by presence of ultramafic lavas
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descriptive term; body is bigger than other part
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intrusive igneous body that cuts across bedding, foliation or structure of county rock into which rock intrudes
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tabular, discordant, intrusive, igneous body
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igneous intrusion whose surfaces are parallel to layering of the intruded rock
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tabular, concordant, intrusive igneous body
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largest dimension is less than 10 times smallest dimension
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