Uranopilite is a secondary uranium sulfate mineral that typically forms as bright yellow, velvety efflorescences on uranium-bearing rocks. It is highly radioactive and recognizable by its intense, vibrant fluorescence under ultraviolet light.
Is this uranopilite?
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 uranopilite with a known reference. Uranopilite 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. Uranopilite leaves a pale yellow streak.
- 3Read the lusterHold the specimen under a strong light. Uranopilite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: yellow, bright yellow, greenish-yellow.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: acicular or fibrous crusts, velvety coatings, spherical aggregates.
Often confused with
Uranopilite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside uranopilite
Minerals reported to co-occur with uranopilite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (UO₂)₆(SO₄)O₂(OH)₆·14H₂O
- Mohs hardness
- 2.5
- Density
- 4.0 g/cm³
- Streak
- Pale Yellow
- Luster
- Pearly
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Acicular or Fibrous Crusts, Velvety Coatings, Spherical Aggregates
- Cleavage
- Perfect
- Fluorescence
- Bright Yellowish-green Under UV Light
- Rarity
- Uncommon
- Uses
- Collector
- Host rock
- Oxidized Uranium Ore Deposits
- Typical price
- $20-150 for small cabinet specimens
Where rockhounds find uranopilite
Classic worldwide localities
- Jachymov, Czech Republic
- Joachimsthal, Czech Republic
- Happy Jack Mine, Utah, USA
- Wheal Owles, Cornwall, UK
Field-hunting tip
Look in oxidized uranium ore deposits country, the host setting where uranopilite typically forms. If you start seeing zippeite, gypsum, johannite in float, you are in the right ground. Field specimens usually show a acicular or fibrous crusts, velvety coatings, spherical aggregates habit, so train your eye for that shape before scanning the outcrop.





