Uralborite is a rare calcium borate mineral primarily found within skarn deposits in contact metamorphic zones. It typically occurs in massive or granular forms and is most notable for its origin in the iron-rich skarn systems of the Ural Mountains.
Is this uralborite?
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 uralborite with a known reference. Uralborite sits at Mohs 4-4.5, 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: colorless.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: granular to massive, occasionally as small prismatic crystals.
Often confused with
Uralborite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside uralborite
Minerals reported to co-occur with uralborite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaB₂O₂(OH)₄
- Mohs hardness
- 4-4.5
- Density
- 2.58-2.60 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Granular to massive, occasionally as small prismatic crystals
- Cleavage
- Indistinct
- Fluorescence
- Violet under LW UV
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A rare secondary mineral in boron-rich iron-ore skarns (Novofrolovskoye deposit, Russia); in a vein cutting limestone (Fuka, Japan)
Where rockhounds find uralborite
Classic worldwide localities
- Novofrolovskoye copper deposit, near Krasnoturinsk, Turinsk district, Northern Ural Mountains, and in the Solongo boron deposit, Buryatia, Russia
- Found at Fuka, near Bicchu, Okayama Prefecture, Japan
Field-hunting tip
Where it forms: A rare secondary mineral in boron-rich iron-ore skarns (Novofrolovskoye deposit, Russia); in a vein cutting limestone (Fuka, Japan). If you start seeing andradite–grossular, magnetite, szaibélyite in float, you are in the right ground. Typical habit: granular to massive, occasionally as small prismatic crystals. Train your eye for that shape before scanning the outcrop.








