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. Streak: light yellow.
- 3Read the lusterHold the specimen under a strong light. Luster: pearly.
- 4Match the color rangeCompare against the expected color range: yellow, orange.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: scaly.
Often confused with
Arsenuranylite vs. its common look-alikes, and how to tell them apart in the field.

How to tell apart: Streak differs, so Arsenuranylite leaves light yellow, Autunite leaves pale yellow; luster reads pearly on Arsenuranylite and vitreous, pearly on {001} on Autunite.

How to tell apart: Luster reads pearly on Arsenuranylite and vitreous to pearly on Phosphuranylite.
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)₄·6H₂O
- Mohs hardness
- 2-3
- Density
- 4.25 g/cm³
- Streak
- Light yellow
- Luster
- Pearly
- Transparency
- Semitransparent
- Crystal system
- Orthorhombic
- Crystal habit
- Scaly
- Cleavage
- One, perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In the oxidized zone of a uranium deposit containing arsenic-bearing sulfides (Cherkasar deposit, Uzbekistan)
Where rockhounds find arsenuranylite
Classic worldwide localities
- Cherkasar uranium deposit, 30 km northwest of Pap, Chatkal Range, Uzbekistan
- Menzenschwand, Black Forest
Field-hunting tip
Where it forms: In the oxidized zone of a uranium deposit containing arsenic-bearing sulfides (Cherkasar deposit, Uzbekistan). If you start seeing paraschoepite, schoepite, metazeunerite in float, you are in the right ground. Typical habit: scaly. Train your eye for that shape before scanning the outcrop.





