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Rock Forming Minerals
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Earljohn Pascua
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Biotite
found in metamorphic and igneous rocks, with a sheet-like structure and weak bonds between layers
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Muscovite
mineral easily identified because its perfect cleavage allows it to be split into thin, flexible, elastic, colorless, transparent sheets with a pearly to vitreous luster
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Calcite
A member of the calcite group, which includes minerals such as aragonite and vaterite
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Garnet
A collection of silicate minerals with similar crystal structures but different chemical compositions
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Biotite
is a highly abundant mineral found in a wide range of igneous and metamorphic rocks.
Biotite minerals
are known for their perfect basal cleavage allowing them to easily separate into thin folia.
Muscovite
is transparent to translucent and usually occur as thin flakes or thicker 'books' of many flakes thickness.
Muscovite
is often formed in metamorphic rocks under low pressure and high temperature conditions, such as schists and gneisses.
Muscovite
is used for
Paint
,
plastics,
rubber,
asphalt
roofing
,
cosmetics
Formation of
calcite
Precipitation from aqueous solutions, biogenic processes, metamorphism
calcite
occurence is in Sedimentary environments, metamorphic environments.
Garnets
are often formed in metamorphic rocks under high pressure and high temperature conditions.
Garnets
are typically found in metamorphic rocks, which are rocks that have undergone significant changes due to intens heat and pressure.