Mineral
Fluorite
Also Known As Fluorspar
Halide Minerals
Fluorite, also called fluorspar, is the mineral form of calcium fluoride, CaF2, and belongs to the halide minerals. It crystallizes in the isometric cubic system, with four perfect cleavage planes that produce octahedral fragments, and the Mohs scale takes it as hardness 4. Pure fluorite is colorless and transparent, but impurities usually make it colorful, and it has been called the most colorful mineral in the world, with purple, blue, green, yellow or colorless the most common shades. It forms as a late-crystallizing mineral in felsic igneous rocks, in hydrothermal vein deposits in limestone and in granitic pegmatites. Industrially it is a flux in steel smelting and a major source of hydrogen fluoride. In 1852 it gave its name to the phenomenon of fluorescence, and it also gave its name to the element fluorine.
Facts
Formation ClassHalide mineral, most commonly forming in hydrothermal veins alongside minerals such as galena, sphalerite, quartz and barite. 1 Chemical Formula Hardness (Mohs) Classification
Strunz Class Crystal System UseOre or Metal Extraction 2 Wikipedia 'Fluorite' states this use (or use-bearing statement); earth5 pass. Connections
Associated With
The Mohs scale defines value 4 as fluorite.
Source Fluorite (Wikipedia)
Fluorite named among the characteristic minerals of complex (rare-element) pegmatites.
Source Pegmatite (Wikipedia)
Caused By
Source Fluorite (Wikipedia)
Source Fluorite (Wikipedia)
Source EBSCO Research Starters: Hydrothermal solutions and mineralization
Additional Source Fluorite (Wikipedia)Occurrence and mining
Classified As
Crystallizes In System
In Discipline
Fluorite is economically significant as a steelmaking flux and as the primary industrial source of fluorine/hydrofluoric acid.
Source Fluorite (Wikipedia)
Source Fluorite (Wikipedia)
In the Other Atlases
Mineral Species Of
Also in Divinity Atlas: of this mineral species.
Sources
1. Fluorite (Wikipedia)
Wikimedia FoundationLead section
Fluorite (also called fluorspar) is the mineral form of calcium fluoride, CaF2. It belongs to the halide minerals. It crystallizes in isometric cubic habit, although octahedral and more complex isometric forms are not uncommon.
Lead section
Fluorite (also called fluorspar) is the mineral form of calcium fluoride, CaF2.
Lead section
It crystallizes in isometric cubic habit, although octahedral and more complex isometric forms are not uncommon.
In Discipline: Economic Geology, Uses section
Metallurgical grade fluorite (60-85% CaF2), the lowest of the three grades, has traditionally been used as a flux to lower the melting point of raw materials in steel production to aid the removal of impurities.
Caused By: Hydrothermal Circulation, Occurrence and mining
Fluorite forms as a late-crystallizing mineral in felsic igneous rocks typically through hydrothermal activity.
Caused By: Fractional Crystallization, Occurrence and mining
Fluorite forms as a late-crystallizing mineral in felsic igneous rocks typically through hydrothermal activity.
Caused By: Hydrothermal Mineral Deposition, Occurrence and mining
It may occur as a vein deposit formed through hydrothermal activity particularly in limestones.
View the Source 2. Wikidata: Fluorite
Wikidata Q102151
3. minerals.net: Fluorite
minerals.netColor field
Fluorite occurs in all colors, including colorless, white, purple, blue, red, pink, orange, yellow, brown, green, gray, and black. May also be multicolored and banded.
Luster field
Vitreous
View the Source 4. Geology.com: Fluorite
Geology.comDescriptionQuote, Description
Fluorite is a common mineral in hydrothermal and carbonate rocks worldwide.
View the Source Pegmatite (Wikipedia)
Wikimedia FoundationAssociated With: Pegmatite, Complex pegmatite mineralogy sectionQuote, Associated With: Pegmatite, Complex pegmatite mineralogy section
These complex pegmatites contain unusual minerals of these elements, such as beryl, spodumene, lepidolite, amblygonite, topaz, apatite, fluorite, tourmaline.
View the Source EBSCO Research Starters: Hydrothermal solutions and mineralization
EBSCO Research StartersCaused By: Hydrothermal Mineral Deposition, Hydrothermal deposit types and gangue mineralsQuote, Caused By: Hydrothermal Mineral Deposition, Hydrothermal deposit types and gangue minerals
Calcite, fluorite, and barite are also common as gangue minerals.
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