Batagayite is an extremely rare phosphate mineral discovered at the Batagay deposit in Russia. It typically occurs as small tabular crystals or radiating aggregates associated with hydrothermal sulfide mineralization. Due to its scarcity, it is almost exclusively found in advanced mineral collections rather than the general market.
Is this batagayite?
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 batagayite with a known reference. Batagayite sits at Mohs 3, 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.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals, radiating aggregates.
Often confused with
Batagayite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside batagayite
Minerals reported to co-occur with batagayite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaZn₂(Zn,Cu)₆(PO₄)₄[PO₃(OH)]₃·12H₂O
- Mohs hardness
- 3
- Density
- 2.90 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular crystals, radiating aggregates
- Cleavage
- Perfect on {001}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A secondary low-temperature mineral formed by alteration of primary minerals (copper and fluorapatite) in a quartz-phosphate mass ~5 m in diameter within greisenized cassiterite-bearing granodiorite
Where rockhounds find batagayite
Classic worldwide localities
- Këster Sn-Ta deposit, Arga-Ynnykh-Khai massif, NE Yakutia, Russia
Field-hunting tip
Where it forms: A secondary low-temperature mineral formed by alteration of primary minerals (copper and fluorapatite) in a quartz-phosphate mass ~5 m in diameter within greisenized cassiterite-bearing granodiorite. If you start seeing copper, arsenolite, tobermorite in float, you are in the right ground. Typical habit: tabular crystals, radiating aggregates. Train your eye for that shape before scanning the outcrop.







