Oursinite is a very rare secondary uranium mineral that typically forms as delicate, needle-like yellow crystals or radial sprays. It is almost exclusively found in association with other rare uranyl minerals in oxidized deposits, making it a highly sought-after but difficult-to-acquire species for radioactive mineral collectors.
Is this oursinite?
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 oursinite with a known reference. Oursinite 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. Oursinite leaves a yellow streak.
- 3Read the lusterHold the specimen under a strong light. Oursinite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, yellowish-green.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: acicular or fibrous radial aggregates.
Often confused with
Oursinite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside oursinite
Minerals reported to co-occur with oursinite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Co(UO₂)₂(SiO₃OH)₂·6H₂O
- Mohs hardness
- 2-3
- Density
- 3.8 g/cm³
- Colors
- Streak
- Yellow
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Acicular or Fibrous Radial Aggregates
- Cleavage
- None
- Fluorescence
- Yellow-green Under UV
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Zones of Uranium Deposits
- Typical price
- $50-500 depending on specimen quality
Where rockhounds find oursinite
Classic worldwide localities
- Shinkolobwe Mine, DR Congo
Field-hunting tip
Look in oxidized zones of uranium deposits country, the host setting where oursinite typically forms. If you start seeing sklodowskite, curite, vandenbrandeite in float, you are in the right ground. Field specimens usually show a acicular or fibrous radial aggregates habit, so train your eye for that shape before scanning the outcrop.





