Uvarovite sits at 6.5–7.5 on the Mohs scale —
harder than glass; scratches steel.
Colors:
Streak White
Crystal system Isometric (Cubic)
SilicatesSilicates (Nesosilicates)
TL;DR · 1 min read
Uvarovite (Ca₃Cr₂(SiO₄)₃) is the chromium end-member of the garnet group and one of the rarest collector garnets. Its brilliant emerald-green color comes from chromium substitution in the garnet structure, and unlike most garnets it almost always occurs as small druzy microcrystal coatings on chromite host rock rather than as large solo crystals.
Uvarovite (Ca₃Cr₂(SiO₄)₃) is the chromium end-member of the garnet group and one of the rarest collector garnets. Its brilliant emerald-green color comes from chromium substitution in the garnet structure, and unlike most garnets it almost always occurs as small druzy microcrystal coatings on chromite host rock rather than as large solo crystals. The Saranovskii Mine in the Ural Mountains of Russia is a major source, supplying iconic emerald-green druzy plates that are display centerpieces in major mineral collections.
Uvarovite is a silicate mineral in the garnet group (ugrandite series) and has the chemical formula Ca3Cr2(SiO4)3. It crystallizes in the isometric system and ranks among the harder species, with lasting durability. Its combination of structural character and global distribution make it a recognized species in both systematic and aesthetic collections.
Identification & care
Uvarovite typically forms small dodecahedral and trapezohedron crystals; drusy crusts on chromite; rarely large enough to facet. The luster is vitreous, adamantine, the streak is white, and specimens range from transparent to translucent. The fracture is conchoidal, uneven, which is one of its key identifying features.
Collector context
How it forms
In terms of geology, Uvarovite forms in chromite deposits in serpentinite/ophiolite complexes; skarns adjacent to chromite lenses; metamorphosed ultrabasic rocks. It is commonly found in association with chromite, serpentine, diopside, calcite, chlorite.
Classic Chinese localities
Uvarovite has known Chinese occurrences in Hebei.
Why collectors care
Uvarovite 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 Uvarovite 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.
Frequently asked questions
What is Uvarovite?
Uvarovite has the chemical formula Ca3Cr2(SiO4)3, crystallises in the Isometric system, has a Mohs hardness of 6.5–7.5. Uvarovite is a silicate mineral recognized for its hardness and durability, with known Chinese sources.
What is the chemical formula of Uvarovite?
The chemical formula of Uvarovite is Ca3Cr2(SiO4)3.
What crystal system does Uvarovite belong to?
Uvarovite crystallises in the Isometric crystal system.
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