Adolfpateraite is a very rare uranyl sulfate mineral originally discovered in the historic silver-mining district of Jáchymov. Collectors will typically find it as small, vibrant yellow crystals associated with other uranium-bearing minerals in hydrothermal vein deposits.
Is this adolfpateraite?
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 adolfpateraite with a known reference. Adolfpateraite 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: pale yellow.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: sulfur-yellow, greenish yellow.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular to prismatic crystals.
Often confused with
Adolfpateraite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside adolfpateraite
Minerals reported to co-occur with adolfpateraite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- K(UO₂)(SO₄)(OH)·H₂O
- Mohs hardness
- ~2
- Density
- 4.24 g/cm³
- Colors
- Sulfur-yellowGreenish yellow
- Streak
- Pale yellow
- Luster
- Vitreous
- Transparency
- Transparent to translucent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular to prismatic crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A secondary mineral in the oxidized zone of a uranium deposit
Where rockhounds find adolfpateraite
Classic worldwide localities
- Geschieber vein, fifth level of the Svornost (Einigkeit) shaft, Jáchymov (Sankt Joachimsthal) ore district, western Bohemia, Czech Republic
Field-hunting tip
Where it forms: A secondary mineral in the oxidized zone of a uranium deposit. If you start seeing gypsum, schoepite, čejkaite in float, you are in the right ground. Typical habit: tabular to prismatic crystals. Train your eye for that shape before scanning the outcrop.




