Arsenuranylite is a rare secondary uranium mineral that typically forms as bright yellow, platy, or micaceous aggregates within the oxidation zones of uranium-bearing hydrothermal veins. Due to its radioactive nature and potential for toxic arsenic exposure, it is intended strictly for professional or experienced collector display.
Is this arsenuranylite?
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 arsenuranylite with a known reference. Arsenuranylite sits at Mohs 2-3, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Arsenuranylite leaves a yellow streak.
- 3Read the lusterHold the specimen under a strong light. Arsenuranylite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: yellow, orange-yellow.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: platy crystals, crusts, radial aggregates.
Often confused with
Arsenuranylite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside arsenuranylite
Minerals reported to co-occur with arsenuranylite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca(UO₂)₄(AsO₄)₂(OH)₄·10H₂O
- Mohs hardness
- 2-3
- Density
- 4.67 g/cm³
- Colors
- Streak
- Yellow
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Platy Crystals, Crusts, Radial Aggregates
- Cleavage
- Perfect On {001}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Uranium Deposits
- Typical price
- $50-300 per specimen depending on size and association
Where rockhounds find arsenuranylite
Classic worldwide localities
- Shinkolobwe mine, DR Congo
- Jáchymov, Czech Republic
- Wheal Gorland, England
Field-hunting tip
Look in oxidized uranium deposits country, the host setting where arsenuranylite typically forms. If you start seeing uraninite, metazeunerite, billietite in float, you are in the right ground. Field specimens usually show a platy crystals, crusts, radial aggregates habit, so train your eye for that shape before scanning the outcrop.






