Uvarovite is the rarest member of the garnet group, instantly recognizable by its distinct, vibrant emerald-green color caused by its chromium content. It is most commonly found as small, brilliant, dodecahedral crystals coating a host rock as a druzy crust, rather than as large, distinct crystals.
Is this uvarovite?
5-step field checkRun through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.
- 1Test the hardnessTry to scratch uvarovite with a known reference. Uvarovite sits at Mohs 6.5-7, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: emerald green, green.
- 5Look at form & habitCrystal system: cubic. Typical habit: crystalline, lamellar.
Often confused with
Uvarovite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside uvarovite
Minerals reported to co-occur with uvarovite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₃Cr₂(SiO₄)₃
- Mohs hardness
- 6.5-7
- Density
- 3.77-3.81 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent to translucent
- Crystal system
- Cubic
- Crystal habit
- Crystalline, lamellar
- Cleavage
- None
- Fluorescence
- Red under SW and LW UV
- Rarity
- Rare
- Uses
- Collector, Lapidary
- Host rock
- From hydrothermal alteration of serpentinite containing chromite; in metamorphosed limestones and skarns from the reaction of dolomite and chromite
Where rockhounds find uvarovite
1 mapped spotsClassic worldwide localities
- Wood's Chrome mine, Lancaster Co., Pennsylvania, USA
- Riddle, Grant Co., Oregon, USA
- Red Ledge mine, near Washington, Nevada Co., around Newcastle, Placer Co., near New Idria, San Benito Co., California, USA
- Saranovskii mine, Biserskoye, in the Gorozavod district, and other localities around Yekaterinburg (Sverdlovsk), Ural Mountains, Russia
- Outokumpu, Finland
- Pico do Posets, near Vénasque, Pyrenees, Spain
Field-hunting tip
Where it forms: From hydrothermal alteration of serpentinite containing chromite; in metamorphosed limestones and skarns from the reaction of dolomite and chromite. If you start seeing chromite, diopside, zoisite in float, you are in the right ground. Typical habit: crystalline, lamellar. Train your eye for that shape before scanning the outcrop. In the U.S., the densest reported localities are in California. Start trip planning there.








