Cobaltite

Cobaltite is a sulfide mineral composed of cobalt, arsenic, and sulfur, CoAsS. Its impurities may contains up to 10% iron and variable amounts of nickel.[5] Structurally, it resembles pyrite (FeS₂) with one of the sulfur atoms replaced by an arsenic atom.

Cobaltite
Cobaltite from Sweden
General
Category	Sulfide mineral
Formula (repeating unit)	CoAsS
Strunz classification	2.EB.25
Crystal system	Orthorhombic
Crystal class	Pyramidal (mm2) (same H-M symbol)
Space group	Pc21b
Unit cell	a = 5.582 Å, b = 5.582 Å, c = 5.582 Å; Z = 4
Identification
Color	Reddish silver white, violet steel gray to black
Crystal habit	Granular to massive, rarely as striated crystals, pseudocubic.
Twinning	About [111] creating pseudo-cubic forms and striations
Cleavage	Perfect on {001}
Fracture	Uneven
Tenacity	Brittle
Mohs scale hardness	5.5
Luster	Metallic
Streak	Grayish-black
Diaphaneity	Opaque
Density	6.33 g/cm3
References	[1][2][3][4]

Although rare, it is mined as a significant source of the strategically important metal cobalt. Secondary weathering incrustations of erythrite, hydrated cobalt arsenate, are common.

The name is from the German, Kobold, "underground spirit" in allusion to the "refusal" of cobaltiferous ores to smelt as they are expected to.[6]

Look up kobold in Wiktionary, the free dictionary.

It occurs in high-temperature hydrothermal deposits and contact metamorphic rocks. It occurs in association with magnetite, sphalerite, chalcopyrite, skutterudite, allanite, zoisite, scapolite, titanite, and calcite along with numerous other Co–Ni sulfides and arsenides.[2] It was described as early as 1832.[3]

It is found chiefly in Sweden, Norway, Germany, Cornwall, England, Canada, La Cobaltera, Chile, Australia, the Democratic Republic of the Congo, and Morocco.[2][5][4]

Cobaltite can be separated from other minerals by selective, pH controlled, flotation methods, where cobalt recovery usually involves hydrometallurgy. It can also be processed with pyrometallurgical methods, such as flash smelting.[7]