Paulscherrerite is a rare uranium oxide mineral that forms as an alteration product of uraninite. It typically presents as small, dull, brownish octahedral crystals often associated with other uranium secondary minerals in hydrothermal deposits.
Is this paulscherrerite?
4-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 paulscherrerite with a known reference. Paulscherrerite sits at Mohs 5-6, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: yellow.
- 3Match the color rangeCompare against the expected color range: canary yellow.
- 4Look at form & habitCrystal system: cubic. Typical habit: octahedral crystals.
Often confused with
Paulscherrerite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside paulscherrerite
Minerals reported to co-occur with paulscherrerite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- UO₂·xH₂O
- Mohs hardness
- 5-6
- Density
- 6.66 g/cm³
- Colors
- Streak
- Yellow
- Transparency
- Translucent
- Crystal system
- Cubic
- Crystal habit
- Octahedral crystals
- Rarity
- Rare
- Uses
- Collector, Scientific research
- Host rock
- A dehydration product of metaschoepite
Where rockhounds find paulscherrerite
Classic worldwide localities
- Number 2 Workings, Radium Ridge, near Arkaroola, Northern Flinders Ranges, South Australia
Field-hunting tip
Where it forms: A dehydration product of metaschoepite. If you start seeing metaschoepite, β-uranophane, weeksite in float, you are in the right ground. Typical habit: octahedral crystals. Train your eye for that shape before scanning the outcrop.



