Zellerite is a rare secondary uranium mineral typically found as fibrous, yellow crusts in oxidized sandstone uranium deposits. It is best identified by its strong green-yellow fluorescence under UV light and its association with other secondary uranium minerals. Due to its radioactive nature, it is primarily sought after by advanced mineral collectors specializing in uranium-bearing species.
Is this zellerite?
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 zellerite with a known reference. Zellerite 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. Zellerite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Zellerite typically shows a earthy luster.
- 4Match the color rangeCompare against the expected color range: yellow, pale yellow.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: fibrous, earthy aggregates, crusts.
Often confused with
Zellerite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside zellerite
Minerals reported to co-occur with zellerite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca(UO₂)(CO₃)₂·5H₂O
- Mohs hardness
- 2
- Density
- 2.5 g/cm³
- Colors
- Streak
- White
- Luster
- Earthy
- Transparency
- Opaque
- Crystal system
- Orthorhombic
- Crystal habit
- Fibrous, Earthy Aggregates, Crusts
- Cleavage
- None
- Fluorescence
- Strong Yellow-green Under UV
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Sedimentary Uranium Deposits in Sandstone
- Typical price
- $50-300 per specimen depending on size and quality
Where rockhounds find zellerite
Classic worldwide localities
- Lucky Mc Mine, Wyoming, USA
- Gas Hills, Wyoming, USA
- Grand County, Utah, USA
Field-hunting tip
Look in sedimentary uranium deposits in sandstone country — that is the host setting where zellerite typically forms. If you start seeing gypsum, meta-autunite, uranyl carbonate minerals in float, you are in the right ground. Field specimens usually show a fibrous, earthy aggregates, crusts habit, so train your eye for that shape before scanning the outcrop.




