Voglite is a rare secondary uranium mineral that forms distinct, vibrant green crusts or small crystalline aggregates in the oxidation zones of uranium deposits. Collectors should look for its association with other uranyl carbonates on oxidized uranium ore, often occurring as delicate, needle-like formations.
Is this voglite?
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 voglite with a known reference. Voglite sits at Mohs 2.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Voglite leaves a pale green streak.
- 3Read the lusterHold the specimen under a strong light. Voglite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: emerald green, grass green.
- 5Look at form & habitCrystal system: triclinic. Typical habit: crusts, granular, acicular aggregates.
Often confused with
Voglite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside voglite
Minerals reported to co-occur with voglite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₂Cu(UO₂)(CO₃)₄·10H₂O
- Mohs hardness
- 2.5
- Density
- 3.0 g/cm³
- Colors
- Streak
- Pale Green
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Triclinic
- Crystal habit
- Crusts, Granular, Acicular Aggregates
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Uranium Ore Deposits
- Typical price
- $50-300 per small specimen
Where rockhounds find voglite
Classic worldwide localities
- Jáchymov, Czech Republic
- Schneeberg, Germany
- Red Canyon, Utah, USA
Field-hunting tip
Look in oxidized uranium ore deposits country — that is the host setting where voglite typically forms. If you start seeing uranyl carbonates, uraninite, gummite in float, you are in the right ground. Field specimens usually show a crusts, granular, acicular aggregates habit, so train your eye for that shape before scanning the outcrop.



