Péligotite is a very rare uranyl sulfate mineral that typically forms as a secondary mineral in oxidized uranium ore deposits. It is best identified by its distinct yellow color and occurrence as thin, platy crystals or crusts associated with other uranium-bearing minerals like zippeite.
Is this péligotite?
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 péligotite with a known reference. Péligotite sits at Mohs 2-3, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Péligotite leaves a yellow streak.
- 3Read the lusterHold the specimen under a strong light. Péligotite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, yellow-green.
- 5Look at form & habitCrystal system: triclinic. Typical habit: platy crystals, crusts.
Often confused with
Péligotite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside péligotite
Minerals reported to co-occur with péligotite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₂UO₂(SO₄)₂·3H₂O
- Mohs hardness
- 2-3
- Density
- 4.2 g/cm³
- Colors
- Streak
- Yellow
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Triclinic
- Crystal habit
- Platy Crystals, Crusts
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Uranium Deposits
- Typical price
- $50-300 per specimen
Where rockhounds find péligotite
Classic worldwide localities
- Jáchymov, Czech Republic
Field-hunting tip
Look in hydrothermal uranium deposits country, the host setting where péligotite typically forms. If you start seeing johannite, zippeite, uraninite in float, you are in the right ground. Field specimens usually show a platy crystals, crusts habit, so train your eye for that shape before scanning the outcrop.



