Kroupaite is a rare uranyl sulfate mineral typically found as a secondary mineral in oxidized uranium deposits. It usually occurs as thin, yellow, platy crystals or as earthy crusts associated with other uranium-bearing secondary minerals. Due to its radioactive nature and scarcity, it is sought primarily by advanced mineral collectors.
Is this kroupaite?
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 kroupaite with a known reference. Kroupaite sits at Mohs ~2, 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: vitreous.
- 4Match the color rangeCompare against the expected color range: orange-yellow.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: platy crystals, crusts, radial aggregates.
Often confused with
Kroupaite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside kroupaite
Minerals reported to co-occur with kroupaite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- KPb₀.₅[(UO₂)₈O₄(OH)₁₀]·10H₂O
- Mohs hardness
- ~2
- Density
- 5.058 g/cm³
- Colors
- Streak
- Light yellow
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Platy crystals, crusts, radial aggregates
- Cleavage
- Perfect on {100}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Of supergene origin by oxidation-hydration alteration of uraninite
Where rockhounds find kroupaite
Classic worldwide localities
- Jan Evangelista vein, Daniel level, Svornost mine, Jáchymov, Western Bohemia, Czech Republic
Field-hunting tip
Where it forms: Of supergene origin by oxidation-hydration alteration of uraninite. If you start seeing fourmarierite, na-rich metaschoepite, uranopilite in float, you are in the right ground. Typical habit: platy crystals, crusts, radial aggregates. Train your eye for that shape before scanning the outcrop.





