Chernikovite is a rare secondary uranium phosphate mineral that typically forms as a dehydration product of autunite. It is characterized by its bright yellow, platy or micaceous crystal habit and exhibits strong green fluorescence under ultraviolet light.
Is this chernikovite?
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 chernikovite with a known reference. Chernikovite sits at Mohs 2-2.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: yellow white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: light yellow.
- 5Look at form & habitCrystal system: tetragonal. Typical habit: micaceous.
Often confused with
Chernikovite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside chernikovite
Minerals reported to co-occur with chernikovite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (H₃O)₂(UO₂)₂(PO₄)₂·6H₂O
- Mohs hardness
- 2-2.5
- Density
- 3.259 g/cm³
- Colors
- Streak
- Yellow white
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Tetragonal
- Crystal habit
- Micaceous
- Cleavage
- Perfect on {001}; imperfect on {010}
- Fluorescence
- Intense yellow green under SW and LW UV
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In fissures in quartz syenite and around fossil wood (Karakat deposit, Tajikistan); along fractures in tourmaline-bearing granites and granite pegmatites (Perus district, Brazil)
Where rockhounds find chernikovite
Classic worldwide localities
- Karakat uranium deposit, 60 km northwest of Khodzhent (Leninabad), Karamazar Mountains, Tajikistan
- Perus district, 25 km north of São Paulo, Brazil
- Rockelmann quarry, near Schwarzenberg, Saxony, and from Ronneburg, Thuringia, Germany
Field-hunting tip
Where it forms: In fissures in quartz syenite and around fossil wood (Karakat deposit, Tajikistan); along fractures in tourmaline-bearing granites and granite pegmatites (Perus district, Brazil). If you start seeing autunite, meta-autunite, sodium autunite in float, you are in the right ground. Typical habit: micaceous. Train your eye for that shape before scanning the outcrop.






