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chapter 6 vocab

Terms

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chemical sedimentary rock
sedimentary rock that forms when minerals precipitate from a solutio n or settle from a suspention
organic sedimentary rock
sedimentary rock that form from the remains of plants or animals
mafic
describes magma or igneouse rock that is rich in magnesium and iron and that is generally dark in color
Brwne's reaction series
the simplifies pattern that illustrates the order in which minerals crystallize from cooling magma according to their chemical composition and melting point
cementation
thge process in which minerals precipitate into pore spaces between sediment grains and bind sediments together to form rock
metamorphism
the process in which one type of rock changes into metamorphic rock because of chemical processes or changes in temerature and pressure
igneous rock
rock that forms when magma cools and solidifies
Rock cycle
the series of processes in which rock forms, change from one type to another, is destroyed,and forms again by geological processes
regional metamorphism
a change in the texyure, structure, or chemical composistion of a rock due to changes in the temperature and pressure over a large area, generally as a result of tectonic forces
clastic sedimentary rock
sedimentary rock that form when fragments of preefixising rocks compacted or cemented together
felsic
describes magma or igneouse rock that is rich in feldspars and silica and that is generally light in color
compaction
the process in which the volume and porosity of a sediment is decreased by the weight of overlying sediments as a result of burial beneath other sediments
intrusive igneous rock
rock formed from the cooling and solitification of magma beneath Earth's surface
contact metamorphism
a change in the texyure, structure, or chemical composistion of a rock due to contact with magma
foliated
the metamorphic rock mineral grains are arranged in planes or bands
extrusive igneouse rock
rock that forms from the cooling and solitification of lava at Earth's surface
nonfoliated
the metamorphic rock mineral grains are not arranged in planes or bands

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