Article · Wikipedia archive · Last revised Jun 28, 2026

Spertiniite

Spertiniite is a rare copper hydroxide mineral. Chemically, it is copper(II) hydroxide with the formula Cu(OH)2. It occurs as blue to blue-green tabular orthorhombic crystal aggregates in a secondary alkaline environment altering chalcocite. Associated minerals include chalcocite, atacamite, native copper, diopside, grossular, and vesuvianite.

Last revised
Jun 28, 2026
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≈ 1 min
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Source
Spertiniite
Spertiniite from Dzhezkazgan, Kazakhstan (size: 5 mm)
General
CategoryOxide mineral
FormulaCu(OH)2
IMA symbolSni1
Strunz classification4.FD.05
Dana classification6.2.4.1
Crystal systemOrthorhombic
Crystal classPyramidal (mm2)
H-M symbol: (mm2)
Space groupCmc21
Unit cella = 2.95 Å, b = 10.59 Å
c = 5.27 Å; Z = 4
Identification
Formula mass97.56 g/mol
ColorBlue, blue-green
Crystal habitFlat tabular crystals occurring in radial to botryoidal aggregates
CleavageNone
TenacityBrittle
Mohs scale hardnessSoft
LusterVitreous
DiaphaneityTransparent
Specific gravity3.93
Optical propertiesBiaxial
Refractive indexnα = 1.720, nβ= n.d., nγ = > 1.800
PleochroismStrong; X = colorless; Z = dark blue
Other characteristicsDecomposes in hot water (synthetic)
References234

Spertiniite is a rare copper hydroxide mineral. Chemically, it is copper(II) hydroxide with the formula Cu(OH)2. It occurs as blue to blue-green tabular orthorhombic crystal aggregates in a secondary alkaline environment altering chalcocite. Associated minerals include chalcocite, atacamite, native copper, diopside, grossular, and vesuvianite.3

Discovery and occurrence

It was first described in 1981 for an occurrence in the Jeffrey Mine of the Johns-Manville mine, Val-des-Sources, Quebec. It was named for mine geologist Francesco Spertini (born 1937).23 In addition to the type locality, it has also been reported from Mont Saint-Hilaire, Quebec; Ely, White Pine County, Nevada; and Bisbee, Cochise County, Arizona. It has been reported from Dzhezkazgan, Kazakhstan; from slag at Juliushutte, Astfeld, Harz Mountains, Germany; and from Tsumeb, Namibia.3

A 2006 study has produced evidence the blue mineral chrysocolla may be a microscopic mixture of spertiniite, amorphous silica and water.56

Crystal structure of spertiniite source ↗
References

References