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Science Chapter 6 vocab.

Terms

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Metamorphism
The process in which one type of rock changes into metamorphic rock because of chemical processes or changes in temperature and pressure.
Regional Metamorphism
A change in the texture, structure, or chemical composition of a rock due to changes in temperature and pressure over a large area, generally as a result of tectonic forces.
Rock Cycle
The series of processes in which rock forms, changes from one type to another, is destroyed, and forms again by geological processes.
Chemical Sedimentary Rock
Sedimentary rock that forms when minerals precipitate from a solution or settle from a suspension.
Extrusive Igneous Rock
Rock that forms from the cooling and solidification of lava at earth's surface.
Intrusive Igneous Rock
Rocked formed from the cooling and solidification of magma beneath Earth's surface.
Organic Sedimentary Rock
Sedimentary rock that the remains of plants or animals.
Compaction
The processing which the volume and porosity of a sediment is decreased by the weight of overlaying sediments as a result of burial beneath other sediments.
Contact Metamorphism
A change in the texture, structure, or chemical composition of a rock due to contact with magma.
Nonfoliated
The metamorphic rock texture in which minerals grains are not arranged in planes or bands.
Mafic
Describes magma or igneous rock that is rich in magnesium and iron and that is generally dark in color
Foliation
The metamorphic rock texture in which mineral grains are arranged in planes or bands.
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.
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.
Cementation
The process in which minerals precipitate into pore spaces between sediment grains and bind sediments together to form rock.

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