Uvite is a calcium-rich member of the tourmaline group, typically forming short, stout prismatic crystals in metamorphosed carbonate rocks. Collectors look for its distinctive trigonal cross-section and its tendency to be associated with contact-metamorphic minerals like diopside and calcite.
Is this uvite?
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 uvite with a known reference. Uvite sits at Mohs 7.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white, light green, light brown.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous to resinous.
- 4Match the color rangeCompare against the expected color range: brown, green, yellow, black, colorless, yellowish brown, blackish brown, bluish black.
- 5Look at form & habitCrystal system: trigonal. Typical habit: prismatic, striated.
Often confused with
Uvite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside uvite
Minerals reported to co-occur with uvite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaMg₃(Al₅Mg)(Si₆O₁₈)(BO₃)₃(OH)₃OH
- Mohs hardness
- 7.5
- Density
- 2.97-3.14 g/cm³
- Streak
- White, light green, light brown
- Luster
- Vitreous to resinous
- Transparency
- Semitransparent
- Crystal system
- Trigonal
- Crystal habit
- Prismatic, striated
- Cleavage
- Indistinct on {1011}
- Fluorescence
- Yellow under SW UV
- Rarity
- Uncommon
- Uses
- Collector, Gemstone, Lapidary
- Host rock
- Typically in calcium-rich rocks subjected to contact metamorphism and metasomatic processes which added boron
Where rockhounds find uvite
1 mapped spotsClassic worldwide localities
- Franklin and Hamburg, Sussex Co., New Jersey, USA
- Gouverneur, Pierrepont, Dekalb, in St. Lawrence Co., and at Horicon, Warren Co., New York, USA
- East Hampton, Middlesex Co., Connecticut, USA
- Uva Province, Sri Lanka
- Sagaing district, Myanmar (Burma)
- Brumado, Bahia, Brazil
Field-hunting tip
Where it forms: Typically in calcium-rich rocks subjected to contact metamorphism and metasomatic processes which added boron. If you start seeing calcite, dolomite, tremolite in float, you are in the right ground. Typical habit: prismatic, striated. Train your eye for that shape before scanning the outcrop. In the U.S., the densest reported localities are in New York. Start trip planning there.








