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science terms

Terms

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extrusive igneous rock
rock that forms from the cooling and solidification of lava at Earth's surface
intrusive igneous rock
rock formed from the cooling and solidification of magma beneath Earth's aurface
foliation
the metamorphic rock texture in which mineral grains are arranged in planes or bands
rock cycle
the series of processes in which rock forms, changes from one type to another, is destroyed, and forms again by geological processes
cementation
the process in which minerals precipitate into pore spaces between sediment grains and bind sediments together to form rock
organic sedimentary rock
sedimentary rock that forms from the remains of plants or animals
contact metamorphism
a change in the texture, structure, or chemical composition of a rock due to contact with magma
regional metamorphism
a change in the texture,structure, or chemical composition of a rock due to changes in tempature and pressure over a large area, generally as a result of tectonic forces
mafic
describes magma or igneous rock that is rich in iron and that is generally dark in color.
chemical sedimentary rock
sedimentary rock that forms when minerals precipitate from a solution or settle from the remains of plants or animals
igneous rock
rock that forms when magma cools and solidifies
clastic sedimentary rock
sedimentary rock that forms when fragments of preexisting rocks are compacted or cemented together
felsic
describes magma or igneous rock that is rich in feldspars and silica and that is generally light in color
nonfoliation
the metamorphic rock texture in which mineral grains are not arranged in planes or bands
compaction
the process in which the volume and porosity of a sediment is decreased by the weight of overlaying sediments as a result of burial beneath other sediments
metamorphism
the process in which one type of rock changes into metamorphic rock because of chemical processes or changes in tempature and pressure
Bowen's reaction series
the simplified pattern that illustrates the order in which minerals crystallize from cooling magma according to their chemical composition and melting point

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