Inesite | |
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Inesite Crystals from Fengjishan Mine (Daye Copper Mine), Edong Mining District, Daye County, Huangshi Prefecture, Hubei Province, China. | |
General | |
Category | Inosilicates |
Formula (repeating unit) | Ca2Mn7Si10O28(OH)2•5(H2O) |
Strunz classification | 09.DL.05 |
Dana classification | 66.3.3.1 |
Crystal system | Triclinic |
Space group | P1 (no.2) |
Identification | |
Color | Rose red, pink, orange-pink, orange-red-brown |
Crystal habit | Massive, fibrous, radial, spherical |
Cleavage | Perfect |
Fracture | Irregular/Uneven |
Tenacity | Brittle |
Mohs scale hardness | 5.5 - 6 |
|re|er}} | Vitreous, Silky |
Streak | White |
Diaphaneity | Translucent |
Specific gravity | 3.0 |
Ultraviolet fluorescence | Non-fluorescent |
Common impurities | Fe, Al, Mg, K |
References | [1][2][3] |
Inesite is a hydrous calcium manganese silicate mineral.[5] Its chemical formula is Ca2Mn7Si10O28(OH)2•5(H2O). Inesite is an inosilicate with a triclinic crystal system. It has a Mohs hardness of 5.5 to 6, and a specific gravity of 3.0. Its name originates from the Greek Ίνες (ines), "fibers" in allusion to its color and habit. [2]
Inesite occurs in hydrothermal replacement deposits of manganese-rich metamorphic rocks and serpentines.[6] It was first described in 1887 at Hilfe Gottes Mine, Oberscheld, Dillenburg, Dillenburg District, Hesse, Germany. Outside of the type locality, there are several notable localities of inesite, such as:[7][8]
Original source: https://en.wikipedia.org/wiki/Inesite.
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