Bobcookite is a rare sodium aluminum uranium sulfate, typically lime-green to greenish yellow. It was approved as a distinct mineral species in 2014. It was first described from Blue Lizard mine, Red Canyon, White Canyon district, San Juan County, Utah, USA.
Is this bobcookite?
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 bobcookite with a known reference. Bobcookite 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: very pale yellowish green.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: lime-green, greenish yellow.
- 5Look at form & habitCrystal system: triclinic. Typical habit: acicular to fibrous sprays or crusts.
Often found alongside bobcookite
Minerals reported to co-occur with bobcookite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- NaAl(UO₂)₂(SO₄)₄·18H₂O
- Mohs hardness
- ~2.5
- Density
- 2.669 g/cm³
- Colors
- Lime-greenGreenish yellow
- Streak
- Very pale yellowish green
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Triclinic
- Crystal habit
- Acicular to fibrous sprays or crusts
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- As efflorescent crusts, on the surfaces of mine walls, derived from the oxidation of primary minerals (uraninite, pyrite, chalcopyrite, bornite and covellite) in a relatively humid underground environment
Where rockhounds find bobcookite
Classic worldwide localities
- Blue Lizard mine, Red Canyon, White Canyon district, San Juan County, Utah, USA
Field-hunting tip
Where it forms: As efflorescent crusts, on the surfaces of mine walls, derived from the oxidation of primary minerals (uraninite, pyrite, chalcopyrite, bornite and covellite) in a relatively humid underground environment. If you start seeing wetherillite, boyleite, chalcanthite in float, you are in the right ground. Typical habit: acicular to fibrous sprays or crusts. Train your eye for that shape before scanning the outcrop.





