Dioptase sits at 5 on the Mohs scale —
can be scratched by a steel knife.
Colors:
Streak Green
Crystal system Trigonal
SilicatesSilicates (Cyclosilicates)
TL;DR · 1 min read
Dioptase (CuSiO₃·H₂O) is a vivid emerald-green copper silicate that ranks among the most visually striking minerals on Earth. Its color rivals gem emerald, and it forms sharp prismatic to rhombohedral crystals in the oxidized cap of copper deposits.
Dioptase (CuSiO₃·H₂O) is a vivid emerald-green copper silicate that ranks among the most visually striking minerals on Earth. Its color rivals gem emerald, and it forms sharp prismatic to rhombohedral crystals in the oxidized cap of copper deposits. Tsumeb (Namibia) and Mindouli/Mfouati (Republic of Congo) produce world-class specimens.
Dioptase is classified as a silicate mineral in the dioptase group and has the chemical formula CuSiO₃·H₂O. It crystallizes in the trigonal system and holds a steady position among silicate species. Its combination of structural character and global distribution make it a recognized species in both systematic and aesthetic collections.
Identification & care
Specimens usually show short prismatic rhombohedral crystals; commonly on matrix. Its color is typically emerald green to blue-green. The luster is sub-adamantine, vitreous, sub-vitreous, the streak is green, and specimens range from transparent to translucent. The cleavage is perfect rhombohedral {1011} in 3 directions. The fracture is conchoidal, which aids identification.
Collector context
How it forms
In terms of geology, Dioptase forms in secondary mineral in oxidized zones of copper ore deposits. It is commonly found in association with wulfenite, malachite, calcite, chrysocolla, shattuckite.
Why collectors care
Dioptase is a frequently-sought species in serious collections because its habit is recognizable, its color often strong, and its best examples unmistakable even at a distance. Chinese material has driven much of the recent visual shift in the species — sharper crystals, deeper colors, cleaner matrix.
What affects value
Value in Dioptase is assessed, in typical order of weight, against: (1) locality provenance; (2) size relative to the species norm; (3) crystal form and termination sharpness; (4) color saturation and zoning; (5) transparency and internal clarity; (6) matrix quality and aesthetic balance; (7) condition (absence of damage, chips, or repair). Cleaning quality and verified locality documentation act as multipliers across the above.
Naming history
Dioptase is Greek for "to see through": dia, through, plus optazein, to see. The name records a moment of mineralogical embarrassment — the first specimens, found in Kazakhstan in the late 18th century, were taken for emerald, and the internal cleavage planes visible through the transparent crystal were what finally gave it away as something else entirely.
Frequently asked questions
What is Dioptase?
Dioptase has the chemical formula CuSiO₃·H₂O, crystallises in the Trigonal system. Dioptase is a silicate mineral recognized among collectors for its crystal form and distribution.
What is the chemical formula of Dioptase?
The chemical formula of Dioptase is CuSiO₃·H₂O.
What crystal system does Dioptase belong to?
Dioptase crystallises in the Trigonal crystal system.
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