Minyulite is a rare hydrated potassium aluminum phosphate typically found as radiating clusters of acicular or prismatic crystals. It is most famous for its occurrence in phosphate-rich nodules, where it forms delicate, often star-shaped, white to colorless sprays.
Is this minyulite?
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 minyulite with a known reference. Minyulite sits at Mohs 3.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Minyulite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Minyulite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: white, colorless, pale yellow.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: acicular or radiating aggregates, prismatic crystals.
Often confused with
Minyulite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside minyulite
Minerals reported to co-occur with minyulite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- KAl₂(PO₄)₂(OH,F)·4H₂O
- Mohs hardness
- 3.5
- Density
- 2.44 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Acicular or Radiating Aggregates, Prismatic Crystals
- Cleavage
- Distinct On {110}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Phosphate-rich Sedimentary Environments, Hydrothermal Veins
- Typical price
- $20-100 per specimen depending on crystal size
Where rockhounds find minyulite
Classic worldwide localities
- Minyulo Well, Western Australia
- Långban, Sweden
- Centerville, South Dakota
- Near Boron, California
Field-hunting tip
Look in phosphate-rich sedimentary environments, hydrothermal veins country — that is the host setting where minyulite typically forms. If you start seeing wavellite, variscite, crandallite in float, you are in the right ground. Field specimens usually show a acicular or radiating aggregates, prismatic crystals habit, so train your eye for that shape before scanning the outcrop.



