BARITE
barite - mineral 28.3.1.1
| Chemical Formula | BaSO4 | |||||||||||||
| Composition | Barium sulfate, sometimes with small amounts of strontium | |||||||||||||
| Variable Formula | (Ba,Sr)SO4 | |||||||||||||
| Color | Colorless, white, yellow, orange, red, brown, blue, gray; sometimes multicolored and banded | |||||||||||||
| Streak | White | |||||||||||||
| Hardness | 3 - 3½ | |||||||||||||
| Crystal Forms and Aggregates |
(Orthorhombic) Most commonly as twinned crystals, which can be quite large. Also occurs tabular, prismatic, and as grainy, platy, and coxcomb aggregates. May also be massive, nodular, fibrous, stalactitic, and as perfect rosettes. | |||||||||||||
| Transparency | Transparent to translucent in thin splinters | |||||||||||||
| Specific Gravity | 4.3 - 4.6 | |||||||||||||
| Luster | Vitreous to pearly | |||||||||||||
| Cleavage | 1,1 - basal ; 2,1 - prismatic ; 3,1 - pinacoidal | |||||||||||||
| Fracture | Uneven | |||||||||||||
| Tenacity | Brittle | |||||||||||||
| Other ID Marks | Commonly fluorescent in a variety of colors, and sometimes also phosphorescent | |||||||||||||
| Other Names | ||||||||||||||
| Varieties | ||||||||||||||
| In Group | Sulfates ; Anhydrous sulfates | |||||||||||||
| All About | Barite is easily
identifiable by its heavy weight, since most similar minerals are much lighter. Barite
often replaces other minerals, and may
even replace organic materials such as wood, shells, and fossils. It sometimes forms tufacious mounds from deposition of hot,
barium-rich springs. Barite specimens from certain locations are brown from sand
inclusions, and may occur in rosette
aggregates that strikingly resemble a flower. Barite is isomorphous with Celestine, and may partially replace it. |
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| Uses | Barite is the main ore of barium. It is also important in the
manufacture of paper, glass, rubber. A rich, white pigment is made from crushed Barite.
Barite is also used in radiology for x-rays of the digestive system. When crushed, it is
added to mud to form barium mud, which is poured into oil wells during drilling. Barite is a very popular mineral among mineral collectors and fine specimens are greatly sought after. |
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| Striking Features | Heaviness, hardness, and crystal habits | |||||||||||||
| Popularity (1-4) | 2 | |||||||||||||
| Prevalence (1-3) | 1 | |||||||||||||
| Demand (1-3) | 1 | |||||||||||||
| Distinguishing Similar Minerals |
Celestine - Very difficult to
distinguish without locality information Calcite - has perfect rhombohedral cleavage, lighter in weight (2.7), and effervesces in hydrochloric acid Fluorite - forms isometric crystals, lighter in weight (3.0 - 3.3) Feldspars - much harder (6), lighter in weight Anglesite - has an adamantine luster |
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| Commonly Occurs With |
Calcite, Fluorite, Chalcopyrite, Cerussite, Gypsum, Anhydrite, Dolomite, Quartz, Apatite, Aragonite, Sulfur | |||||||||||||
| Noteworthy Localities |
On a worldwide basis, fine
specimens have come from a number of areas in Australia, Belgium, England, and Morocco. In the U.S., yellow, tabular Barite associated with Fluorite comes from Sterling, Weld Co., Colorado. It is also found with Fluorite in Cave In Rock, Hardin Co., Illinois. Other localities include Nye Co., Nevada; Alpine Co., California; Palos Verdes Hills, Los Angeles Co., California; Leadville, Lake Co., Colorado; and Elk Creek, Mead Co., South Dakota. Large, lustrous, golden-yellow crystals come from the Barrick Meickle Mine in Eureka County (near Carlin). Perfect "roses" have come from the vicinity of Norman, Cleveland Co., Oklahoma, and from the Sahara Desert in Africa. |
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| Picture
Icon Links |
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| Picture Links | 1.Yelow coxcomb Barite | 2.Colorless, transparent Barite | 3.White, coxcomb Barite with Chalcopyrite | 4.Barite Desert Rose | 5.Green, prismatic Barite | 6.Tabular orange crystals |
Additional references
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