Shumwayite is a rare uranyl sulfate mineral typically found as small, vibrant yellow tabular crystals in oxidized uranium deposits. It is best identified through its association with other secondary uranium minerals and its occurrence in arid mining environments. Due to its radioactivity and solubility, it requires careful storage in a dry environment.
Is this shumwayite?
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 shumwayite with a known reference. Shumwayite 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. Shumwayite leaves a yellow streak.
- 3Read the lusterHold the specimen under a strong light. Shumwayite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, yellow-green.
- 5Look at form & habitCrystal system: triclinic. Typical habit: tabular crystals, radial aggregates.
Often confused with
Shumwayite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside shumwayite
Minerals reported to co-occur with shumwayite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- UO₂(SO₄)·5H₂O
- Mohs hardness
- 2
- Density
- 3.31 g/cm³
- Colors
- Streak
- Yellow
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Triclinic
- Crystal habit
- Tabular Crystals, Radial Aggregates
- Cleavage
- Good
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Zones of Uranium Mines
- Typical price
- $50-300 per specimen
Where rockhounds find shumwayite
Classic worldwide localities
- Hillside mine, Yavapai County, Arizona, USA
Field-hunting tip
Look in oxidized zones of uranium mines country — that is the host setting where shumwayite typically forms. If you start seeing gypsum, halotrichite, johannite in float, you are in the right ground. Field specimens usually show a tabular crystals, radial aggregates habit, so train your eye for that shape before scanning the outcrop.




