Leószilárdite is a rare uranyl carbonate mineral typically found as small, bright yellow tabular crystals or crusts in uranium-bearing sandstone. It was discovered in the San Rafael Swell of Utah and is highly prized by advanced collectors for its rarity and complex chemical composition.
Is this leószilárdite?
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 leószilárdite with a known reference. Leószilárdite 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. Leószilárdite leaves a pale yellow streak.
- 3Read the lusterHold the specimen under a strong light. Leószilárdite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals, crusts.
Often confused with
Leószilárdite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside leószilárdite
Minerals reported to co-occur with leószilárdite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₆Mg(UO₂)₂(CO₃)₆·6H₂O
- Mohs hardness
- 2
- Density
- 2.98 g/cm³
- Colors
- Streak
- Pale Yellow
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular Crystals, Crusts
- Cleavage
- Good
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Sedimentary Sandstone
- Typical price
- $50-300 thumbnail
Where rockhounds find leószilárdite
Classic worldwide localities
- San Rafael Swell, Utah, USA
Field-hunting tip
Look in sedimentary sandstone country, the host setting where leószilárdite typically forms. If you start seeing uraninite, gypsum in float, you are in the right ground. Field specimens usually show a tabular crystals, crusts habit, so train your eye for that shape before scanning the outcrop.




