Korzhinskite is a rare calcium borate mineral typically found in boron-rich skarn deposits. It often forms thin, platy, or radial crystal clusters that can be difficult to distinguish from other borate species without advanced testing.
Is this korzhinskite?
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 korzhinskite with a known reference. Korzhinskite sits at Mohs 3.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Korzhinskite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Korzhinskite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: white, colorless.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: platy crystals, radial aggregates.
Often confused with
Korzhinskite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside korzhinskite
Minerals reported to co-occur with korzhinskite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaB₂O₄·H₂O
- Mohs hardness
- 3.5
- Density
- 3.1 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Platy Crystals, Radial Aggregates
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Skarn Deposits
- Typical price
- $50-300 per specimen
Where rockhounds find korzhinskite
Classic worldwide localities
- Sakha Republic, Russia
- Solongo deposit, Buryatia, Russia
Field-hunting tip
Look in skarn deposits country — that is the host setting where korzhinskite typically forms. If you start seeing calcite, ludwigite, suanite in float, you are in the right ground. Field specimens usually show a platy crystals, radial aggregates habit, so train your eye for that shape before scanning the outcrop.






