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science vocab

Terms

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Organic sedimentary rock
Sedimentary rock that forms from the remains of plants or animals.
intrusive igneauos rock
rock formed from the cooling and solidification of magma beneath earths surface
Metamorphism
The process in which one type of rock changes into metamorphic rock because of chemical processes or changes in temperature and pressure.
Igneous Rock
Rock that forms when magma cools and solidifies.
Intrusive igneous rock
Rock formed from the cooling and solidification of magma beneath Earth's surface.
Regional metamorphism
A change in the texture structure or chemical composition of a rock due to changes in tem. And pressure over a large area generally as a result of tectonic forces
Compaction
The process in which the volume and porosity of a sediment of a sediment is decreased by the weight of overlying sediments as a result of burial beneath other sediments.
Cementation
The process in which minerals precipitate into pore spaces between sediment grains and bind sediments together to form rock.
Mafic
Describe magma or igneous rock that is rich in magnesium and iron and that is generally dark in color.
Felsic
Describe magma or igneous rock that id rich in feldspars and silica and that is generally light in color.
Clastic sedimentary rock
Sedimentary rock that forms when fragments of preexisting rocks are compacted or cemented together.
Chemical sedimentary rock
Sedimentary rock that forms when minerals precipitation from a solution or settle from a suspension
Rock cycle
The series of processes in which rocks form changes from one type to another, is destroyed and again by geological processes.
Extrusive igneous rock
Rock that forms from the cooling and solidification of lava at Earth's surface.
Contact metamorphism
A change in the texture, structure, or chemical composition of a rock due to contact with magma.
compaction
the process in wihich a form of sedimentary rock is formed over another form of sesdimentary rock so that they are opposite layers
Browns 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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