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| the series of processes in which rock forms, changes from one type to another, is destroyed, and forms again by geologicla processess |
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| the simpified pattern that illustartes the order in which minerals crystallize form cooling magma according to thier chemical and melting point |
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| rock that forms when magma cools and solidifies |
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| roack formed from the cooling and solidification of magma beneath Earth's surface |
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| rock that forms from the cooling and soldification of lava at Earth's surface |
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| describes magma or igneous rock that is rich in feldspar and silica and that is generally light in color |
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| describes magma or igneous rock that is rich in magnesium and iron and that is generally dark in color |
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| the process in which the volume and porosity of a sediment is decreased by the wieght of overlying sediments as a result of burial beneath other sediments |
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| the process in which minerals precipitate into pore spaces between sediment grains and bind sediments together to form rock |
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| chemical sedimentary rock |
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| sedimentary roack that forms when minerals precipitate froma solution or settle from a suspension |
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| sedimentary rock that forms from the remains of the plants or animals |
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| sedimentary rock that forms when fragments of preexsisting roack that are compacted together |
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| the process in which one type of rock changes into metamorphic rock because of the chemiacl processes or changes in temperature and pressure |
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| a change in the texture, structure, or chemical composition of a rock due to contact with magma |
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| a change in the texture, structure, or chemical composition of a rock due to changes in temperatureand pressure over a large area, generally as a result of tectonic forces |
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| the metamorphic rocj texture in which mineral grains are arranged in planes or brands |
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| the metamorphic rock texture in which mineral grains aer not arranged in planes or bands |
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