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. Mitryaevaite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Mitryaevaite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: white, colorless.
- 5Look at form & habitCrystal system: triclinic. Typical habit: tabular crystals, radiating aggregates.
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
- (Al,Fe³⁺)₇(PO₄)₄(SO₄,SiO₄)(OH,F)₁₂·8H₂O
- Mohs hardness
- 3-4
- Density
- 2.44 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Triclinic
- Crystal habit
- Tabular Crystals, Radiating Aggregates
- Cleavage
- Good
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Sedimentary Phosphate Deposits
- Typical price
- n/a
Where rockhounds find mitryaevaite
Classic worldwide localities
- Karatau Mountains, Kazakhstan
Field-hunting tip
Look in sedimentary phosphate deposits country — that is the host setting where mitryaevaite typically forms. If you start seeing quartz, goethite, crandallite in float, you are in the right ground. Field specimens usually show a tabular crystals, radiating aggregates habit, so train your eye for that shape before scanning the outcrop.





