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Tephroite is uncommon member of the Olivine group. It is the manganese counterpart of Forsterite, and forms a series with Forsterite. Tephroite gets it name from the Greek word "tephros", meaning ash-colored, referring to its ash-gray color habit.
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Chemical Formula |
Mn2SiO4 |
Composition |
Manganese silicate, sometimes with some magnesium and zinc. Forms a series with Forsterite. |
Variable Formula |
(Mn,Mg,Zn)2SiO4 |
Color |
Gray, grayish-green, olive-green, brown, reddish-brown, pink |
Streak |
Light gray |
Hardness |
6 |
Crystal System |
Orthorhombic |
Crystal Forms and Aggregates |
As rounded and fractured crystals, usually short and prismatic, but occasionally elongated. Also occurs grainy, massive, and in large cleavage fragments. |
Transparency |
Translucent. Rarely transparent. |
Specific Gravity |
4.0 - 4.1 |
Luster |
Vitreous, greasy, waxy |
Cleavage |
2,1 ; 3,1- forming a 90º angle |
Fracture |
Conchoidal to uneven |
Tenacity |
Brittle |
In Group |
Silicates; Nesosilicates |
Striking Features |
Cleavage angles, color, and hardness. |
Environment |
In manganese-rich metamorphic deposits. |
Rock Type |
Metamorphic |
Popularity (1-4)
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3 |
Prevalence (1-3)
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3 |
Demand (1-3) |
3 |
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Worldwide localities for Tephroite include Broken Hill, New South Wales, Australia; the Wessels Mine, Hotazel, Kalahari manganese fields, South Africa; and Langban, Sweden. In the U.S., the most well-known Tephroite is from Franklin, Ogdensburg, and Sparta, all in Sussex Co., New Jersey. Tephroite is also found in the Jail Hill Quarry, Haddam, Middlesex Co., Connecticut.
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Willemite - Different cleavage, fluoresces bright green. Rhodonite - Usually pinker in color.
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