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, 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.







