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 — that is 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.



