Urancalcarite is a rare secondary uranium mineral that typically forms as delicate, radiating tufts of acicular crystals. It is primarily found in the oxidized zones of uranium deposits and is highly prized by collectors for its brilliant neon-yellow fluorescence under UV light.
Is this urancalcarite?
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 urancalcarite with a known reference. Urancalcarite 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: light yellow.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: bright yellow.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: acicular, aggregates, radial.
Often confused with
Urancalcarite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside urancalcarite
Minerals reported to co-occur with urancalcarite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca(UO₂)₃CO₃(OH)₆·3H₂O
- Mohs hardness
- 2-3
- Density
- 4.03 g/cm³
- Colors
- Streak
- Light yellow
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Acicular, aggregates, radial
- Cleavage
- None
- Fluorescence
- Bright yellow-green under UV light
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In the oxidation zone of uranium deposits
Where rockhounds find urancalcarite
Classic worldwide localities
- Found at an undisclosed locality in Hunan Province, China
Field-hunting tip
Where it forms: In the oxidation zone of uranium deposits. If you start seeing uraninite, uranophane, wyartite in float, you are in the right ground. Typical habit: acicular, aggregates, radial. Train your eye for that shape before scanning the outcrop.





