Natropharmacoalumite is a rare secondary mineral typically occurring as small, transparent, pseudocubic crystals in the oxidized zones of arsenic-rich ore deposits. It is structurally related to the pharmacosiderite group and is most easily identified by its occurrence in specific secondary mineral assemblages alongside other arsenic-bearing species.
Is this natropharmacoalumite?
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 natropharmacoalumite with a known reference. Natropharmacoalumite 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. Natropharmacoalumite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Natropharmacoalumite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: white, colorless, pale yellow.
- 5Look at form & habitCrystal system: cubic. Typical habit: pseudocubic crystals.
Often confused with
Natropharmacoalumite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside natropharmacoalumite
Minerals reported to co-occur with natropharmacoalumite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- NaAl₄(AsO₄)₃(OH)₄·4H₂O
- Mohs hardness
- 2.5
- Density
- 2.56 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Cubic
- Crystal habit
- Pseudocubic Crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Arsenic-rich Hydrothermal Deposits
- Typical price
- $50-300 per specimen depending on size and quality
Where rockhounds find natropharmacoalumite
Classic worldwide localities
- Jáchymov, Czech Republic
- Gold Hill, Utah, USA
- Laurion, Greece
Field-hunting tip
Look in oxidized arsenic-rich hydrothermal deposits country — that is the host setting where natropharmacoalumite typically forms. If you start seeing arsenopyrite, scorodite, pharmacosiderite in float, you are in the right ground. Field specimens usually show a pseudocubic crystals habit, so train your eye for that shape before scanning the outcrop.





