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, 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.



