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, 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.





