Schoepite is a secondary uranium mineral that forms through the alteration of uraninite in the oxidation zone of uranium-rich deposits. It is frequently found as bright yellow, tabular crystals or crusts that are strongly radioactive and should be handled with care.
Is this schoepite?
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 schoepite with a known reference. Schoepite 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. Schoepite leaves a yellow streak.
- 3Read the lusterHold the specimen under a strong light. Schoepite typically shows a adamantine luster.
- 4Match the color rangeCompare against the expected color range: yellow, amber-yellow.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: tabular crystals, often as crusts or powdery aggregates.
Often confused with
Schoepite vs. its common look-alikes, and how to tell them apart in the field.


How to tell apart: Luster reads adamantine on Schoepite and vitreous on Billietite.

How to tell apart: Curite is the harder of the two (Mohs 4-5 vs. 2.5); streak differs, so Schoepite leaves yellow, Curite leaves orange.
Often found alongside schoepite
Minerals reported to co-occur with schoepite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- [(UO₂)₈O₂(OH)₁₂]·12H₂O
- Mohs hardness
- 2.5
- Density
- 4.8 g/cm³
- Colors
- Streak
- Yellow
- Luster
- Adamantine
- Transparency
- Translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Tabular Crystals, Often as Crusts or Powdery Aggregates
- Cleavage
- Perfect in One Direction
- Fluorescence
- Yellow-green Under UV
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Zone of Uranium Deposits
- Typical price
- $50-500 depending on specimen quality and size
Where rockhounds find schoepite
Classic worldwide localities
- Democratic Republic of the Congo
- Czech Republic
- Canada
- Germany
- USA
Field-hunting tip
Look in oxidized zone of uranium deposits country, the host setting where schoepite typically forms. If you start seeing uraninite, becquerelite, curite in float, you are in the right ground. Field specimens usually show a tabular crystals, often as crusts or powdery aggregates habit, so train your eye for that shape before scanning the outcrop.


