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. Feynmanite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Feynmanite typically shows a vitreous luster.
- 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
- Na₂UO₂(SO₄)₂·2H₂O
- Mohs hardness
- 2
- Density
- 2.81 g/cm³
- 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
- Typical price
- $50-300 per specimen
Where rockhounds find feynmanite
Classic worldwide localities
- Repete Mine, Utah, USA
Field-hunting tip
Look in uranium-bearing sedimentary rocks country — that is the host setting where feynmanite typically forms. If you start seeing johannite, zippeite, gypsum 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.



