Paddlewheelite is a very rare uranyl carbonate mineral typically found as small, vibrant yellow platy crystals or crusts. It is named for its unique crystal structure that resembles a paddlewheel. It is predominantly found in the historic mining district of Jáchymov, Czech Republic, associated with other secondary uranium minerals.
Is this paddlewheelite?
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 paddlewheelite with a known reference. Paddlewheelite 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. Paddlewheelite leaves a yellow streak.
- 3Read the lusterHold the specimen under a strong light. Paddlewheelite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, greenish-yellow.
- 5Look at form & habitCrystal system: triclinic. Typical habit: platy crystals, crusts.
Often confused with
Paddlewheelite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside paddlewheelite
Minerals reported to co-occur with paddlewheelite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- MgCu₂(UO₂)₂(CO₃)₃(OH)₄·18H₂O
- Mohs hardness
- 2
- Density
- 3.55 g/cm³
- Colors
- Streak
- Yellow
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Triclinic
- Crystal habit
- Platy Crystals, Crusts
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Veins
- Typical price
- $50-300 per thumbnail specimen
Where rockhounds find paddlewheelite
Classic worldwide localities
- Jáchymov, Czech Republic
Field-hunting tip
Look in hydrothermal veins country — that is the host setting where paddlewheelite typically forms. If you start seeing uraninite, liebigite, andersonite in float, you are in the right ground. Field specimens usually show a platy crystals, crusts habit, so train your eye for that shape before scanning the outcrop.




