Uranopolycrase is a rare radioactive member of the euxenite group, typically found as an accessory mineral in granite pegmatites. It often presents as dark, metallic-looking prismatic crystals that are frequently metamict due to internal radiation damage.
Is this uranopolycrase?
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 uranopolycrase with a known reference. Uranopolycrase sits at Mohs 5.5-6.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Uranopolycrase leaves a brownish-yellow streak.
- 3Read the lusterHold the specimen under a strong light. Uranopolycrase typically shows a submetallic luster.
- 4Match the color rangeCompare against the expected color range: black, brownish-black.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: prismatic, tabular, or massive.
Often confused with
Uranopolycrase vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside uranopolycrase
Minerals reported to co-occur with uranopolycrase. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Y,Ca,Ce,U,Th)(Nb,Ta,Ti)₂O₆
- Mohs hardness
- 5.5-6.5
- Density
- 5.1-5.5 g/cm³
- Colors
- Streak
- Brownish-yellow
- Luster
- Submetallic
- Transparency
- Opaque
- Crystal system
- Orthorhombic
- Crystal habit
- Prismatic, Tabular, Or Massive
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Granite Pegmatites
- Typical price
- $50-500 depending on specimen size and radioactivity levels
Where rockhounds find uranopolycrase
Classic worldwide localities
- Norway
- Madagascar
- Canada
- USA
Field-hunting tip
Look in granite pegmatites country, the host setting where uranopolycrase typically forms. If you start seeing monazite, zircon, feldspar in float, you are in the right ground. Field specimens usually show a prismatic, tabular, or massive habit, so train your eye for that shape before scanning the outcrop.





