Feynmanite is a very rare uranyl sulfate mineral discovered in the oxidized zone of uranium mines. It typically forms small, vibrant yellow tabular crystals or crusts that are highly fluorescent under specific conditions and require careful handling due to radioactivity.
Is this feynmanite?
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 feynmanite with a known reference. Feynmanite 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: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: yellow, yellowish-green.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals, crusts.
Often confused with
Feynmanite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside feynmanite
Minerals reported to co-occur with feynmanite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na(UO₂)(SO₄)(OH)·3.5H₂O
- Mohs hardness
- 2
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular crystals, crusts
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- uranium-bearing sedimentary rocks
Where rockhounds find feynmanite
Classic worldwide localities
- Repete Mine, Utah, USA
Field-hunting tip
Where it forms: uranium-bearing sedimentary rocks. If you start seeing johannite, zippeite, gypsum in float, you are in the right ground. Typical habit: tabular crystals, crusts. Train your eye for that shape before scanning the outcrop.



