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spherocobaltite
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spherocobaltite

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Spherocobaltite or sphaerocobaltite is the mineral form of Cobalt(II) carbonate (). It is a cobalt bearing member of the calcite group of carbonate minerals, crystallizing in the trigonal crystal system. Rare specimens of pure spherocobaltite typically show a rose-red color, but the color range of impure specimens extends to shades of pink and pale brown.

Key facts

Mineral.name
Spherocobaltite
Mineral.category
Carbonate mineral
Mineral.image
Sphaerocobaltite.jpg
Mineral.caption
Spherocobaltite from Peramea, Lérida, Catalonia, Spain
Mineral.formula
CoCO3
Mineral.IMAsymbol
Scbt
Mineral.molweight
118.94 g/mol
Mineral.strunz
5.AB.05
Mineral.system
Trigonal
Mineral.class
Hexagonal scalenohedral (m) H-M symbol: ( 2/m)
Mineral.symmetry
Rc
Mineral.unit cell
a = 4.65, c = 14.95 [Å]; Z = 6
Mineral.color
Most commonly dark magenta red; pink to red, brown, brownish red, grey, greyish red, velvet-black (due to surface alteration)
Mineral.habit
Encrustations - forms crust-like aggregates on matrix, crystals uncommon: rhombohedral to discoidal
Mineral.cleavage
Perfect rhomboidal cleavage
Mineral.mohs
4
Mineral.luster
Vitreous
Mineral.refractive
nε = 1.600, nω = 1.885

via Wikipedia infobox

Wikidata facts

Image
Spherocobaltite-112780.jpg
Show 6 more facts
chemical formula
CoCO₃
Nickel-Strunz 9th edition (updated 2009)
5.AB.05
Commons category
Spherocobaltite
Nickel-Strunz '10th ed', review of (9th ed/ 2009 update)
5.AB.05
IMA Mineral Symbol
Scbt
Strunz 8th edition (series ID, updated)
Vb/A.02
Sources (1)

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Article

3 sections
Contents
  • Discovery and occurrence
  • References
  • Further reading

Spherocobaltite or sphaerocobaltite is the mineral form of Cobalt(II) carbonate (). It is a cobalt bearing member of the calcite group of carbonate minerals, crystallizing in the trigonal crystal system. Rare specimens of pure spherocobaltite typically show a rose-red color, but the color range of impure specimens extends to shades of pink and pale brown.

==Discovery and occurrence== Spherocobaltite was first described in 1877 for an occurrence within cobalt and nickel veins in the St. Daniel Mine of the Schneeberg District, Ore Mountains, Saxony, Germany. The name is from the Greek "sphaira", sphere, and cobalt, in reference to its typical crystal habit and composition. It occurs within hydrothermal cobalt-bearing mineral deposits as a rare phase associated with roselite, erythrite, annabergite and cobalt rich calcite and dolomite.

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