Sibirskite is a rare calcium borate mineral typically found in metamorphosed carbonate rocks associated with skarn deposits. It usually occurs as small, white to colorless platy or fibrous crystalline aggregates. It is primarily a collector's mineral known from the Tayozhnoye iron ore deposit in the Sakha Republic of Russia.
Is this sibirskite?
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 sibirskite with a known reference. Sibirskite sits at Mohs 3-4, 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, dark gray.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: platy or fibrous aggregates.
Often confused with
Sibirskite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside sibirskite
Minerals reported to co-occur with sibirskite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaHBO₃
- Mohs hardness
- 3-4
- Density
- 2.58 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Semitransparent
- Crystal system
- Monoclinic
- Crystal habit
- Platy or fibrous aggregates
- Cleavage
- Good
- Rarity
- Rare
- Uses
- Collector, Research
- Host rock
- In veinlets and aggregates in skarns
Where rockhounds find sibirskite
Classic worldwide localities
- Yuliya Svintsovaya Pb–Zn deposit, 20 km east-northeast of the Son railway station, Khakassia district, Siberia, Russia
- Novofrolovskoye copper deposit, near Krasnoturinsk, Turinsk district, Northern Ural Mountains, Russia
- Chersk and Selenyakhsk Ridges, Transbaikal, Russia
- Fuka, near Bicchu, Okayama Prefecture, Japan
Field-hunting tip
Where it forms: In veinlets and aggregates in skarns. If you start seeing calcite, chlorite, pyrite in float, you are in the right ground. Typical habit: platy or fibrous aggregates. Train your eye for that shape before scanning the outcrop.








