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fluor-uvite

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Also known as Fluvt

Fluor-uvite is a tourmaline mineral with the chemical formula CaMg3(Al5Mg)(Si6O18)(BO3)3(OH)3F. It is a rare mineral that is found in calcium rich contact metamorphic rocks with increased amounts of boron. Uvite is trigonal hexagonal, which means that it has three equal length axes at 120 degrees, all perpendicular to its fourth axis which has a different length. Uvite is part of the space group 3m. Uvite's hardness has been measured to be 7.5 on the Mohs hardness scale. The color of uvite widely varies, depending on the sample, but is mostly deep green or brown. In regard to uvite's optical p

Key facts

Mineral.imagesize
260px
Mineral.name
Fluor-uvite
Mineral.category
Cyclosilicatetourmaline group
Mineral.image
Uvite sur quartz (Brésil) 4.JPG
Mineral.caption
Uvite on quartz
Mineral.formula
CaMg3(Al5Mg)(Si6O18)(BO3)3(OH)3F
Mineral.IMAsymbol
Fluvt
Mineral.strunz
9.CK.05
Mineral.system
Trigonal
Mineral.class
Ditrigonal pyramidal (3m) H-M symbol: (3m)
Mineral.symmetry
R3m
Mineral.color
Black, greenish-black, brownish-black, brown, green, colorless
Mineral.cleavage
None Observed
Mineral.fracture
Irregular/Uneven, Conchoidal
Mineral.tenacity
Brittle
Mineral.mohs
7.5
Mineral.luster
Vitreous, Resinous
Mineral.opticalprop
Uniaxial (-)

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Wikidata facts

Image
Uvite-155037.jpg
Show 5 more facts
Commons category
Uvite
Nickel-Strunz '10th ed', review of (9th ed/ 2009 update)
9.CK.05
Nickel-Strunz 9th edition (updated 2009)
9.CK.05
IMA Mineral Symbol
Fluvt
chemical formula
CaMg₃(Al₅Mg)(Si₆O₁₈)(BO₃)₃(OH)₃F
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Fluor-uvite is a tourmaline mineral with the chemical formula CaMg3(Al5Mg)(Si6O18)(BO3)3(OH)3F. It is a rare mineral that is found in calcium rich contact metamorphic rocks with increased amounts of boron. Uvite is trigonal hexagonal, which means that it has three equal length axes at 120 degrees, all perpendicular to its fourth axis which has a different length. Uvite is part of the space group 3m. Uvite's hardness has been measured to be 7.5 on the Mohs hardness scale. The color of uvite widely varies, depending on the sample, but is mostly deep green or brown. In regard to uvite's optical properties, it is uniaxial (-) and anisotropic, meaning that the velocity of light in the mineral depends on the path that it takes. In plane polarized light, uvite is colorless to pale yellow and shows weak pleochroism.

Uvite was first found in 1929 in Uva Province, Sri Lanka, hence the name.

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