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 — that is 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.




