Šreinite is a rare uranyl phosphate mineral typically found as small, yellow, platy crystals or thin crusts. It is most commonly associated with primary uranium deposits and weathered hydrothermal veins, specifically documented in the historic mining region of Jáchymov.
Is this šreinite?
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 šreinite with a known reference. Šreinite sits at Mohs 2-4, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: pale yellow.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous to sub-adamantine.
- 4Match the color rangeCompare against the expected color range: yellow with an orange tint.
- 5Look at form & habitCrystal system: cubic. Typical habit: platy crystals, crusts.
Often confused with
Šreinite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside šreinite
Minerals reported to co-occur with šreinite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pb(UO₂)₄(BiO)₃(PO₄)₂(OH)₇·4H₂O
- Mohs hardness
- 2-4
- Density
- 5.20 g/cm³
- Colors
- Yellow with an orange tint
- Streak
- Pale yellow
- Luster
- Vitreous to sub-adamantine
- Transparency
- Opaque
- Crystal system
- Cubic
- Crystal habit
- Platy crystals, crusts
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A secondary mineral
Where rockhounds find šreinite
Classic worldwide localities
- Horní Hale, Krune Hory Mts., Czech Republic (type locality)
Field-hunting tip
Where it forms: A secondary mineral. If you start seeing uranosphaerite, goethite, pb-bearing phosphuranylite in float, you are in the right ground. Typical habit: platy crystals, crusts. Train your eye for that shape before scanning the outcrop.







