Pertsevite-(OH) is a rare magnesium borate mineral first discovered in the contact-metasomatic boron deposits of the Tayozhnoye iron deposit in Siberia. It typically occurs as small tabular crystals or intergrown grains within magnesium-rich skarn environments. Due to its rarity and specific formation conditions, it is primarily sought after by advanced systematic mineral collectors.
Is this pertsevite-(oh)?
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 pertsevite-(oh) with a known reference. Pertsevite-(OH) sits at Mohs 5-6 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Pertsevite-(OH) leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Pertsevite-(OH) typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, white.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: tabular crystals, anhedral grains.
Often confused with
Pertsevite-(OH) vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside pertsevite-(oh)
Minerals reported to co-occur with pertsevite-(oh). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Mg₂BO₃(OH)
- Mohs hardness
- 5-6
- Density
- 3.31 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Tabular Crystals, Anhedral Grains
- Cleavage
- None Observed
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Boron-bearing Skarns
- Typical price
- $50-300 for rare micro-specimens
Where rockhounds find pertsevite-(oh)
Classic worldwide localities
- Tayozhnoye deposit, Aldan Shield, Russia
Field-hunting tip
Look in boron-bearing skarns country — that is the host setting where pertsevite-(oh) typically forms. If you start seeing magnetite, forsterite, suanite in float, you are in the right ground. Field specimens usually show a tabular crystals, anhedral grains habit, so train your eye for that shape before scanning the outcrop.






