Tyretskite is a rare borate mineral typically found in sedimentary salt sequences and evaporite basins. Collectors should look for its tabular monoclinic crystals in saline beds, often associated with other borate species and evaporite minerals.
Is this tyretskite?
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 tyretskite with a known reference. Tyretskite sits at Mohs 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: white, brownish, brownish white.
- 5Look at form & habitCrystal system: triclinic. Typical habit: tabular crystals, massive.
Often confused with
Tyretskite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside tyretskite
Minerals reported to co-occur with tyretskite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₂B₅O₉(OH)·H₂O
- Mohs hardness
- 5
- Density
- 2.189 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Triclinic
- Crystal habit
- Tabular crystals, massive
- Cleavage
- Good
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Cavity in dolomitic saline rock, in drillcore from a depth of 1233 m
Where rockhounds find tyretskite
Classic worldwide localities
- Tyret railway station, on the east Siberian railway, in the Lena-Angara salt basin, Irkutsk district, Siberia, Russia (type locality)
Field-hunting tip
Where it forms: Cavity in dolomitic saline rock, in drillcore from a depth of 1233 m. If you start seeing halite, gypum, anhydrite in float, you are in the right ground. Typical habit: tabular crystals, massive. Train your eye for that shape before scanning the outcrop.




