Pharmacoalumite is a rare secondary arsenic mineral that typically forms small, pseudocubic crystals in the oxidized zones of ore deposits. It is chemically similar to pharmacosiderite but features aluminum instead of iron in its structure, resulting in lighter, often yellowish or greenish hues.
Is this pharmacoalumite?
3-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 pharmacoalumite with a known reference. Pharmacoalumite sits at Mohs 2.5, softer than the next harder reference, harder than the previous one.
- 2Match the color rangeCompare against the expected color range: white.
- 3Look at form & habitCrystal system: cubic. Typical habit: pseudocubic crystals, crusts, or massive.
Often confused with
Pharmacoalumite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside pharmacoalumite
Minerals reported to co-occur with pharmacoalumite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- KAl₄(AsO₄)₃(OH)₄·6.5H₂O
- Mohs hardness
- 2.5
- Density
- 2.676 g/cm³
- Colors
- Transparency
- Translucent
- Crystal system
- Cubic
- Crystal habit
- Pseudocubic crystals, crusts, or massive
- Cleavage
- Imperfect on {100}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A secondary mineral with other oxidized arsenates on a museum specimen
Where rockhounds find pharmacoalumite
Classic worldwide localities
- Germany
- United Kingdom
- USA
- France
Field-hunting tip
Where it forms: A secondary mineral with other oxidized arsenates on a museum specimen. If you start seeing ceruleite, olivenite, schlossmacherite in float, you are in the right ground. Typical habit: pseudocubic crystals, crusts, or massive. Train your eye for that shape before scanning the outcrop.






