Trolleite is a rare phosphate mineral often found in high-pressure metamorphic environments. It typically appears as pale blue-green or white massive aggregates, frequently associated with other aluminum phosphates like lazulite and augelite.
Is this trolleite?
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 trolleite with a known reference. Trolleite sits at Mohs 5.5-6 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Trolleite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Trolleite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: pale green, blue-green, white, colorless.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: massive, granular, rarely as small pseudo-hexagonal crystals.
Often confused with
Trolleite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside trolleite
Minerals reported to co-occur with trolleite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Al₄(PO₄)₃(OH)₃
- Mohs hardness
- 5.5-6
- Density
- 3.10 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Massive, Granular, Rarely as Small Pseudo-hexagonal Crystals
- Cleavage
- Distinct On {110}
- Rarity
- Rare
- Uses
- Collector, Lapidary
- Host rock
- Metamorphic Rocks Rich in Aluminum and Phosphorus
- Typical price
- $20-150 for small specimens, higher for gem-grade rough
Where rockhounds find trolleite
Classic worldwide localities
- Västanå mine, Sweden
- Rapid Creek, Yukon, Canada
- Champion mine, California, USA
- Minas Gerais, Brazil
Field-hunting tip
Look in metamorphic rocks rich in aluminum and phosphorus country — that is the host setting where trolleite typically forms. If you start seeing augelite, attakolite, lazulite in float, you are in the right ground. Field specimens usually show a massive, granular, rarely as small pseudo-hexagonal crystals habit, so train your eye for that shape before scanning the outcrop.







