Čejkaite is an extremely rare secondary uranium carbonate mineral found primarily in the Jachymov mining district. It typically forms thin tabular crystals or delicate crusts and is identified by its association with other secondary uranium minerals in oxidized zones.
Is this čejkaite?
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 čejkaite with a known reference. Čejkaite 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. Streak: light yellow.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: pale yellow, beige.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: microscopic crystals, pseudo hexagonal.
Often confused with
Čejkaite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside čejkaite
Minerals reported to co-occur with čejkaite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₄(UO₂)(CO₃)₃
- Mohs hardness
- 2
- Density
- 3.67 g/cm³
- Colors
- Streak
- Light yellow
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Microscopic crystals, pseudo hexagonal
- Fluorescence
- Weak yellow under SW UV; weak greenish yellow under LW UV
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Secondary mineral associated with decomposed uraninite
Where rockhounds find čejkaite
Classic worldwide localities
- Jachymov, NW Bohemia, Czech Republic (type locality)
Field-hunting tip
Where it forms: Secondary mineral associated with decomposed uraninite. If you start seeing andersonite, schröckingerite in float, you are in the right ground. Typical habit: microscopic crystals, pseudo hexagonal. Train your eye for that shape before scanning the outcrop.



