Mitryaevaite is a rare phosphate mineral first discovered in the Karatau phosphorite deposits of Kazakhstan. It typically forms delicate, colorless to white tabular crystals or radiating sprays within sedimentary phosphate environments.
Is this mitryaevaite?
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 mitryaevaite with a known reference. Mitryaevaite 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, dull in massive nodules.
- 4Match the color rangeCompare against the expected color range: white, colorless.
- 5Look at form & habitCrystal system: triclinic. Typical habit: encrustations, nodular, pulverulent.
Often confused with
Mitryaevaite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside mitryaevaite
Minerals reported to co-occur with mitryaevaite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Al₅(PO₄)₂[(P,S)O₃(OH,O)]₂F₂(OH)₂·14.5H₂O
- Mohs hardness
- 3-4
- Density
- 2.02 g/cm³
- Streak
- White
- Luster
- Vitreous, dull in massive nodules
- Transparency
- Transparent in microcrystals
- Crystal system
- Triclinic
- Crystal habit
- Encrustations, nodular, pulverulent
- Cleavage
- On {001}, perfect; on {010}, {100}, good
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A secondary mineral in fractures and veinlets, in altered and oxidized vanadium-bearing phosphatic black shales
Where rockhounds find mitryaevaite
Classic worldwide localities
- Kurumsak Formation, from the Taldyk mining district, northwestern Kara-Tau Range to the Zhabagly Mountains, Tien-Shan, southern Kazakhstan
Field-hunting tip
Where it forms: A secondary mineral in fractures and veinlets, in altered and oxidized vanadium-bearing phosphatic black shales. If you start seeing minyulite, crandallite, gorceixite in float, you are in the right ground. Typical habit: encrustations, nodular, pulverulent. Train your eye for that shape before scanning the outcrop.








