Waylandite is a rare phosphate mineral typically occurring as small, crusty, or globular masses. It is primarily sought after by advanced collectors for its rarity and its characteristic association with phosphate minerals in hydrothermal or pegmatite environments.
Is this waylandite?
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 waylandite with a known reference. Waylandite sits at Mohs 4-5, 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 to dull.
- 4Match the color rangeCompare against the expected color range: white, light brown.
- 5Look at form & habitCrystal system: trigonal. Typical habit: crusts, globular aggregates, microscopic crystals.
Often confused with
Waylandite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside waylandite
Minerals reported to co-occur with waylandite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- BiAl₃(PO₄)₂(OH)₆
- Mohs hardness
- 4-5
- Density
- 3.86 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous to dull
- Transparency
- Translucent
- Crystal system
- Trigonal
- Crystal habit
- Crusts, globular aggregates, microscopic crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A rare secondary mineral replacing primary bismuth minerals
Where rockhounds find waylandite
Classic worldwide localities
- Wampewo pegmatite, Gamba Hill, near Kampala, southwest Uganda
- Ngusa, and in the Kobokobo pegmatite, Lusungu River district, Kivu Province, Congo (Zaire)
- Restormel mine, near Lostwithiel, England
- Wheal Owles and the Levant mine, St. Just, England
- Phoenix mines, near Linkinhorne, England
- Gunheath china clay pit, St. Austell, Cornwall, England
Field-hunting tip
Where it forms: A rare secondary mineral replacing primary bismuth minerals. If you start seeing bismutite, bismutotantalite in float, you are in the right ground. Typical habit: crusts, globular aggregates, microscopic crystals. Train your eye for that shape before scanning the outcrop.





