Sakhaite is a rare borate mineral found almost exclusively in contact metasomatic skarn deposits. It is best identified by its bright yellow fluorescence under shortwave UV light and its occurrence alongside other magnesium-borate species.
Is this sakhaite?
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 sakhaite with a known reference. Sakhaite 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 to slightly greasy.
- 4Match the color rangeCompare against the expected color range: colorless, gray, gray white.
- 5Look at form & habitCrystal system: cubic. Typical habit: euhedral crystals, massive.
Often confused with
Sakhaite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside sakhaite
Minerals reported to co-occur with sakhaite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₄₈Mg₁₆(BO₃)₃₂(CO₃)₁₆·2(H₂O,HCl)
- Mohs hardness
- 5
- Density
- 2.78-2.83 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous to slightly greasy
- Transparency
- Transparent
- Crystal system
- Cubic
- Crystal habit
- Euhedral crystals, massive
- Cleavage
- None
- Fluorescence
- Bright yellow under SW UV
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In lenses replacing marble at the contact of a granitic massif with dolostone (Titovskoye deposit, Russia)
Where rockhounds find sakhaite
Classic worldwide localities
- Titovskoye boron deposit, Tas-Khayakhtakh Mountains, Sakha, and at the Solongo boron deposit, Buryatia, Russia
- Sayak-IV boron deposit, northeast Balkhash region, Kazakhstan
- Daiy Mountain, Qiliping, Hunan Province, China
- Fuka, near Bicchu, Okayama Prefecture, Japan
- Kombat Cu–Pb–Ag mine, 49 km south of Tsumeb, Namibia
Field-hunting tip
Where it forms: In lenses replacing marble at the contact of a granitic massif with dolostone (Titovskoye deposit, Russia). If you start seeing kotoite, clinohumite, forsterite in float, you are in the right ground. Typical habit: euhedral crystals, massive. Train your eye for that shape before scanning the outcrop.







