Stanleyite is a rare hydrated vanadium sulfate mineral typically found as vibrant green, 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 2 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Stanleyite leaves a pale green streak.
- 3Read the lusterHold the specimen under a strong light. Stanleyite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: bright green, yellow-green.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: acicular crystals, fibrous, crusts.
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
- V⁴⁺O(SO₄)·5H₂O
- Mohs hardness
- 2
- Density
- 3.32 g/cm³
- Colors
- Streak
- Pale Green
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Acicular Crystals, Fibrous, Crusts
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Zones of Vanadium-bearing Sulfide Deposits
- Typical price
- $50-300 per specimen
Where rockhounds find stanleyite
Classic worldwide localities
- Ragra mine, Peru
- Kazakhstan
Field-hunting tip
Look in oxidized zones of vanadium-bearing sulfide deposits country — that is the host setting where stanleyite typically forms. If you start seeing quisqueite, patronite, melanterite in float, you are in the right ground. Field specimens usually show a acicular crystals, fibrous, crusts habit, so train your eye for that shape before scanning the outcrop.


