Oppenheimerite is a rare copper sodium sulfate mineral first identified at the Rowley Mine in Arizona. It typically appears as small, vibrant yellow tabular crystals formed in the oxidation zones of ore deposits.
Is this oppenheimerite?
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 oppenheimerite with a known reference. Oppenheimerite sits at Mohs 2.5, 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: pale greenish yellow.
- 5Look at form & habitCrystal system: triclinic. Typical habit: tabular crystals.
Often confused with
Oppenheimerite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside oppenheimerite
Minerals reported to co-occur with oppenheimerite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₂(UO₂)(SO₄)₂·3H₂O
- Mohs hardness
- 2.5
- Density
- 3.360 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Triclinic
- Crystal habit
- Tabular crystals
- Cleavage
- Good on {11̄0}, {011} and {101}
- Fluorescence
- Bright yellow-green under UV
- Rarity
- Rare
- Uses
- Collector
- Host rock
- oxidized mine dumps and hydrothermal veins
Where rockhounds find oppenheimerite
Classic worldwide localities
- Blue Lizard mine, Red Canyon, White Canyon district, San Juan County, Utah, USA
Field-hunting tip
Where it forms: oxidized mine dumps and hydrothermal veins. If you start seeing fermiite, blödite, bluelizardite in float, you are in the right ground. Typical habit: tabular crystals. Train your eye for that shape before scanning the outcrop.






