Stanleyite is a rare hydrated vanadium sulfate mineral typically found as aquamarine-blue to deep cobalt-blue, needle-like crystals or crusts. It forms as a secondary mineral in the oxidation zones of vanadium-rich sulfide deposits. Due to its solubility, it is best kept in a dry environment to prevent dehydration.
Is this stanleyite?
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 stanleyite with a known reference. Stanleyite sits at Mohs 1-1.5, 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: blue, deep blue.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: crystalline, efflorescences.
Often confused with
Stanleyite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside stanleyite
Minerals reported to co-occur with stanleyite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- VO(SO₄)·6H₂O
- Mohs hardness
- 1-1.5
- Density
- 1.95 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Semitransparent
- Crystal system
- Orthorhombic
- Crystal habit
- Crystalline, efflorescences
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Initially found on a museum specimen of patronite from a rich vanadium deposit
Where rockhounds find stanleyite
Classic worldwide localities
- Minasragra, 46 km from Cerro de Pasco, Peru
Field-hunting tip
Where it forms: Initially found on a museum specimen of patronite from a rich vanadium deposit. If you start seeing patronite, pyrite, potassium alum in float, you are in the right ground. Typical habit: crystalline, efflorescences. Train your eye for that shape before scanning the outcrop.



