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 — that is 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.





