Plavnoite is a rare secondary uranium sulfate mineral typically found as a yellow crust or powdery coating on weathered uranium-bearing ores. It is primarily known from the Jáchymov region and is of interest primarily to advanced mineral collectors focusing on uranium species.
Is this plavnoite?
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 plavnoite with a known reference. Plavnoite 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. Plavnoite leaves a yellow streak.
- 3Read the lusterHold the specimen under a strong light. Plavnoite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, golden yellow.
- 5Look at form & habitCrystal system: triclinic. Typical habit: microcrystalline crusts, earthy aggregates.
Often confused with
Plavnoite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside plavnoite
Minerals reported to co-occur with plavnoite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- K₂Mn(UO₂)₂(SO₄)₄·8H₂O
- Mohs hardness
- 2.5
- Density
- 3.32 g/cm³
- Colors
- Streak
- Yellow
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Triclinic
- Crystal habit
- Microcrystalline Crusts, Earthy Aggregates
- Cleavage
- None Observed
- Rarity
- Rare
- Uses
- Collector, Scientific Research
- Host rock
- Hydrothermal Uranium Deposits
- Typical price
- $50-300 per specimen depending on size and quality
Where rockhounds find plavnoite
Classic worldwide localities
- Jáchymov, Czech Republic
- Plavno, Czech Republic
Field-hunting tip
Look in hydrothermal uranium deposits country — that is the host setting where plavnoite typically forms. If you start seeing uraninite, johannite, gypsum in float, you are in the right ground. Field specimens usually show a microcrystalline crusts, earthy aggregates habit, so train your eye for that shape before scanning the outcrop.





