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. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: colorless.
- 5Look at form & habitCrystal system: triclinic. Typical habit: bladed.
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
- 5.36 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Semitransparent
- Crystal system
- Triclinic
- Crystal habit
- Bladed
- Cleavage
- Perfect on {100}, good on {010}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In the oxidized zone of an epithermal Cu–Pb–Ag deposit
Where rockhounds find artroeite
Classic worldwide localities
- Grand Reef mine, near Klondyke, Aravaipa district, Graham Co., Arizona, USA
Field-hunting tip
Where it forms: In the oxidized zone of an epithermal Cu–Pb–Ag deposit. If you start seeing calcioaravaipaite, quartz, anglesite in float, you are in the right ground. Typical habit: bladed. Train your eye for that shape before scanning the outcrop.








