Claudetite is a rare monoclinic form of arsenic trioxide that often forms as thin, delicate, platy crystals in the oxidized zones of arsenic-rich ore bodies. Due to its toxicity and delicate nature, it is strictly a mineral for advanced collectors and should be stored in a sealed container.
Is this claudetite?
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 claudetite with a known reference. Claudetite 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. Claudetite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Claudetite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: white, colorless.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: platy or thin tabular crystals, crusts, fan-like aggregates.
Often confused with
Claudetite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside claudetite
Minerals reported to co-occur with claudetite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- As₂O₃
- Mohs hardness
- 2.5
- Density
- 4.0 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Platy or Thin Tabular Crystals, Crusts, Fan-like Aggregates
- Cleavage
- Perfect in One Direction
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Zones of Arsenic-rich Hydrothermal Deposits
- Typical price
- $20-150 for thumbnail to small cabinet specimens
Where rockhounds find claudetite
Classic worldwide localities
- Jáchymov, Czech Republic
- Banská Štiavnica, Slovakia
- Cerro de Pasco, Peru
- Eureka, Utah, USA
Field-hunting tip
Look in oxidized zones of arsenic-rich hydrothermal deposits country — that is the host setting where claudetite typically forms. If you start seeing arsenopyrite, realgar, orpiment in float, you are in the right ground. Field specimens usually show a platy or thin tabular crystals, crusts, fan-like aggregates habit, so train your eye for that shape before scanning the outcrop.





