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Rhodonite - Wikipedia

From Wikipedia, the free encyclopedia

Single chain manganese inosilicate (MnSiO3)

Rhodonite

Rhodonite from San Martín Mine, Chiurucu, Huallanca District, Bolognesi Province,

Ancash

,

Peru

Specimen size: 53 mm × 52 mm × 40 mm (2.1 in × 2.0 in × 1.6 in)

Category Inosilicate Formula (Mn2+, Fe2+, Mg, Ca)SiO3 IMA symbol Rdn[1] Strunz classification 9.DK.05 Dana classification 65.04.01.01 Crystal system Triclinic Crystal class Pinacoidal (1)
(same H–M symbol) Space group P1 Unit cell a = 9.758 Å, b = 10.499 Å, c = 12.205 Å; α = 108.58°, β = 102.92°, γ = 82.52°; Z = 20 Color Pink, rose-pink to brownish red, red, gray and yellow Crystal habit Tabular crystals, massive, granular Twinning Lamellar, composition plane {010} Cleavage Perfect on {110} and {110}, (110) ^ (110) = 92.5°; good on {001} Fracture Conchoidal to uneven Mohs scale hardness 5.5–6.5 Luster Vitreous to pearly Streak White Diaphaneity Transparent to translucent Specific gravity 3.57–3.76 Optical properties Biaxial (+) Refractive index nα = 1.711–1.738, nβ = 1.714–1.741, nγ = 1.724–1.751 Birefringence δ = 0.013 Pleochroism Weak 2V angle 58° to 73° (measured), 58° (calculated) Alters to Exterior commonly black from manganese oxides References [2][3][4]

Rhodonite is a manganese inosilicate, with the formula (Mn, Fe, Mg, Ca)SiO3, and member of the pyroxenoid group of minerals, crystallizing in the triclinic system. It commonly occurs as cleavable to compact masses with a rose-red color (its name comes from Ancient Greek ῥόδον (rhódon) 'rose'), often tending to brown due to surface oxidation. The rose-red hue is caused by the manganese cation (Mn2+).[5]

Rhodonite crystals often have a thick tabular habit, but are rare. It has a perfect, prismatic cleavage, almost at right angles. The hardness is 5.5–6.5, and the specific gravity is 3.4–3.7; luster is vitreous, being less frequently pearly on cleavage surfaces. The manganese is often partly replaced by iron, magnesium, calcium, and sometimes zinc, which may sometimes be present in considerable amounts; a greyish-brown variety containing as much as 20% of calcium oxide is called bustamite; fowlerite is a zinciferous variety containing 7% of zinc oxide.

Pink rhodonite contrasting with black manganese oxides is sometimes used as gemstone material as seen in this specimen from Humboldt County, Nevada.

The inosilicate (chain silicate) structure of rhodonite has a repeat unit of five silica tetrahedra. The rare polymorph pyroxmangite, formed at different conditions of pressure and temperature, has the same chemical composition but a repeat unit of seven tetrahedra.

Rhodonite has also been worked as an ornamental stone. In the iron and manganese mines at Pajsberg near Filipstad and Långban in Värmland, Sweden, small brilliant and translucent crystals (pajsbergite) and cleavage masses occur. Fowlerite occurs as large, rough crystals, somewhat resembling pink feldspar, with franklinite and zinc ores in granular limestone at Franklin Furnace in New Jersey.

Rhodonite is the official gemstone of the Commonwealth of Massachusetts.[6]

 This article incorporates text from a publication now in the public domainChisholm, Hugh, ed. (1911). "Rhodonite". Encyclopædia Britannica (11th ed.). Cambridge University Press.

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Gemstones

Gemmological classifications by E. Ya. Kievlenko (1980), updated

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