Artroeite is an extremely rare lead aluminum fluoride hydroxide mineral known primarily from the oxidized zone of the Mammoth-St. Anthony mine. It typically occurs as small, colorless to white tabular crystals and is prized by micro-mineral collectors for its rarity and crystal structure.
Is this artroeite?
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 artroeite with a known reference. Artroeite sits at Mohs 2.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Artroeite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Artroeite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, white.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals.
Often confused with
Artroeite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside artroeite
Minerals reported to co-occur with artroeite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- PbAlF₃(OH)₂
- Mohs hardness
- 2.5
- Density
- 5.68 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular Crystals
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Lead-bearing Ore Deposits
- Typical price
- $50-300 per thumbnail
Where rockhounds find artroeite
Classic worldwide localities
- Mammoth-St. Anthony mine, Arizona, USA
Field-hunting tip
Look in oxidized lead-bearing ore deposits country — that is the host setting where artroeite typically forms. If you start seeing cerussite, anglesite, wulfenite in float, you are in the right ground. Field specimens usually show a tabular crystals habit, so train your eye for that shape before scanning the outcrop.






