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 3 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Kroupaite leaves a yellow streak.
- 3Read the lusterHold the specimen under a strong light. Kroupaite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: yellow, 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
- K₂[UO₂(SO₄)₂]·nH₂O
- Mohs hardness
- 3
- Density
- 4.92 g/cm³
- Colors
- Streak
- Yellow
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Platy Crystals, Crusts, Radial Aggregates
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Uranium Veins
- Typical price
- $50-300 per specimen
Where rockhounds find kroupaite
Classic worldwide localities
- Jáchymov, Czech Republic
- Loděnice, Czech Republic
Field-hunting tip
Look in hydrothermal uranium veins country — that is the host setting where kroupaite typically forms. If you start seeing uraninite, gummite, uranopilite in float, you are in the right ground. Field specimens usually show a platy crystals, crusts, radial aggregates habit, so train your eye for that shape before scanning the outcrop.


