Augelite is a rare phosphate mineral often found as attractive, transparent, wedge-shaped crystals. It is highly prized by collectors for its clarity and aesthetic crystal habits, though it is typically found in small, localized deposits.
Is this augelite?
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 augelite with a known reference. Augelite sits at Mohs 4.5-5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Augelite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Augelite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, white, yellowish, pale pink, pale green.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular to prismatic crystals, often wedge-shaped.
Often confused with
Augelite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside augelite
Minerals reported to co-occur with augelite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Al₂PO₄(OH)₃
- Mohs hardness
- 4.5-5
- Density
- 2.70 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular to Prismatic Crystals, Often Wedge-shaped
- Cleavage
- Perfect On {110}, Distinct On {011}
- Rarity
- Rare
- Uses
- Collector, Gemstone
- Host rock
- Hydrothermal Veins and Metamorphic Rocks
- Typical price
- $20-200 per specimen
Where rockhounds find augelite
Classic worldwide localities
- Baden, Germany
- Oruro Department, Bolivia
- Rapid Creek, Yukon, Canada
- White Mountains, California, USA
Field-hunting tip
Look in hydrothermal veins and metamorphic rocks country, the host setting where augelite typically forms. If you start seeing quartz, pyrophyllite, lazulite in float, you are in the right ground. Field specimens usually show a tabular to prismatic crystals, often wedge-shaped habit, so train your eye for that shape before scanning the outcrop.







