Plášilite is a rare secondary uranium mineral typically found as small, pale blue tabular crystals in oxidized hydrothermal veins. It is known primarily from the Jáchymov district in the Czech Republic and is highly sought after by collectors specializing in rare uranyl minerals.
Is this plášilite?
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 plášilite with a known reference. Plášilite 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. Plášilite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Plášilite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: blue, pale blue.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals, crusts.
Often confused with
Plášilite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside plášilite
Minerals reported to co-occur with plášilite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na(UO₂)(SeO₄)(OH)·2H₂O
- Mohs hardness
- 2
- Density
- 3.51 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular Crystals, Crusts
- Cleavage
- Good
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Uranium-rich Vein Deposits
- Typical price
- $100-500 thumbnail size
Where rockhounds find plášilite
Classic worldwide localities
- Jachymov, Czech Republic
Field-hunting tip
Look in hydrothermal uranium-rich vein deposits country — that is the host setting where plášilite typically forms. If you start seeing haynesite, ferro-celadonite, uranyl sulfates in float, you are in the right ground. Field specimens usually show a tabular crystals, crusts habit, so train your eye for that shape before scanning the outcrop.


