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 6.5-7.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Uvarovite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Uvarovite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: emerald green.
- 5Look at form & habitCrystal system: isometric. Typical habit: dodecahedral crystals, granular, massive, drusy.
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
- 6.5-7.5
- Density
- 3.4-3.8 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Isometric
- Crystal habit
- Dodecahedral Crystals, Granular, Massive, Drusy
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector, Lapidary
- Host rock
- Metamorphosed Chromite-bearing Serpentinites
- Typical price
- $20-200 for specimens depending on crystal size and matrix quality
Where rockhounds find uvarovite
1 mapped spotsClassic worldwide localities
- Outokumpu (Finland)
- Sarany (Russia)
- San Benito County (USA)
- Transvaal (South Africa)
Field-hunting tip
Look in metamorphosed chromite-bearing serpentinites country — that is the host setting where uvarovite typically forms. If you start seeing chromite, calcite, diopside in float, you are in the right ground. Field specimens usually show a dodecahedral crystals, granular, massive, drusy habit, so 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.






