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 — 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 — that is 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.


