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, 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.


