Oswaldpeetersite is a rare uranyl carbonate mineral typically found as delicate, vibrant yellow lath-like crystals. It is primarily known from the Musonoi Mine in the Congo and is highly sought after by collectors specializing in secondary uranium minerals due to its intense fluorescence under UV light.
Is this oswaldpeetersite?
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 oswaldpeetersite with a known reference. Oswaldpeetersite 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. Streak: pale yellow.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: canary yellow.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: microscopic crystals, prismatic.
Often confused with
Oswaldpeetersite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside oswaldpeetersite
Minerals reported to co-occur with oswaldpeetersite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (UO₂)₂CO₃(OH)₂·4H₂O
- Mohs hardness
- 2-3
- Density
- 4.54 g/cm³
- Colors
- Streak
- Pale yellow
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Microscopic crystals, prismatic
- Cleavage
- Parallel elongation
- Fluorescence
- Bright green under SW UV
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In a sedimentary Colorado-Plateau-type U–V deposit
Where rockhounds find oswaldpeetersite
Classic worldwide localities
- Jomac uranium mine, Brown’s Rim, White Canyon district, San Juan Co., Utah, USA
Field-hunting tip
Where it forms: In a sedimentary Colorado-Plateau-type U–V deposit. If you start seeing gypsum, cuprite, antlerite in float, you are in the right ground. Typical habit: microscopic crystals, prismatic. Train your eye for that shape before scanning the outcrop.








