Wyllieite is a rare phosphate mineral typically found as a primary or secondary phase in complex granite pegmatites. It is often identified by its distinct green to brownish hues and its occurrence alongside other phosphate minerals like triphylite. Collectors generally look for it in classic pegmatite localities where it forms small, well-defined prismatic crystals or massive aggregates.
Is this wyllieite?
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 wyllieite with a known reference. Wyllieite sits at Mohs 4-4.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: olive green.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous to submetallic.
- 4Match the color rangeCompare against the expected color range: dark green, bluish green, greenish black, gray green.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: prismatic crystals, massive, granular.
Often confused with
Wyllieite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside wyllieite
Minerals reported to co-occur with wyllieite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₂Mn²⁺(Fe²⁺,Fe³⁺)Al(PO₄)₃
- Mohs hardness
- 4-4.5
- Density
- 3.601 g/cm³
- Streak
- Olive green
- Luster
- Vitreous to submetallic
- Transparency
- Semitransparent
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic crystals, massive, granular
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In zoned complex granite pegmatites
Where rockhounds find wyllieite
Classic worldwide localities
- Old Mike mine, six km north-northwest of Custer, Custer Co., South Dakota, USA
- Buranga pegmatite, near Gatumba, Rwanda
- Hålsjöberg, Värmland, Sweden
- Lavra do Énio pegmatite, northeast of Galiléia, Minas Gerais, Brazil
Field-hunting tip
Where it forms: In zoned complex granite pegmatites. If you start seeing trolleite, scorzalite in float, you are in the right ground. Typical habit: prismatic crystals, massive, granular. Train your eye for that shape before scanning the outcrop.



