Znucalite is a very rare secondary uranium-zinc carbonate mineral that forms as thin, pearly crusts or small platy crystals in oxidized zones. It is highly valued by mineral collectors for its distinct bright green fluorescence under shortwave ultraviolet light.
Is this znucalite?
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 znucalite with a known reference. Znucalite sits at Mohs 2 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Znucalite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Znucalite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: white, colorless, pale yellow.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: platy crystals, crusts, aggregates.
Often confused with
Znucalite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside znucalite
Minerals reported to co-occur with znucalite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaZn₁₁(UO₂)₂(CO₃)₃(OH)₂₂·4H₂O
- Mohs hardness
- 2
- Density
- 2.8 g/cm³
- Streak
- White
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Platy Crystals, Crusts, Aggregates
- Cleavage
- Perfect in One Direction
- Fluorescence
- Bright Green Under SW UV
- Rarity
- Rare
- Uses
- Collector, Scientific Study
- Host rock
- Oxidized Zones of Uranium-zinc Hydrothermal Deposits
- Typical price
- $50-300 per specimen
Where rockhounds find znucalite
Classic worldwide localities
- Jachymov, Czech Republic
- Schneeberg, Germany
- Rum Jungle, Australia
Field-hunting tip
Look in oxidized zones of uranium-zinc hydrothermal deposits country — that is the host setting where znucalite typically forms. If you start seeing adamite, smithsonite, uraninite in float, you are in the right ground. Field specimens usually show a platy crystals, crusts, aggregates habit, so train your eye for that shape before scanning the outcrop.




