Vanalite is a rare secondary vanadium mineral that typically forms as soft, yellow to orange-yellow crusts in sandstone. It is most commonly identified in oxidation zones of uranium-vanadium mines in the Colorado Plateau, where it appears in microscopic aggregates.
Is this vanalite?
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 vanalite with a known reference. Vanalite sits at Mohs 1 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Vanalite leaves a yellow streak.
- 3Read the lusterHold the specimen under a strong light. Vanalite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: yellow, yellow-orange.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: crusts, aggregates of lath-like crystals.
Often confused with
Vanalite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside vanalite
Minerals reported to co-occur with vanalite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Al₄V₂O₂V₄O₁₂(OH)₄·11H₂O
- Mohs hardness
- 1
- Density
- 2.51 g/cm³
- Colors
- Streak
- Yellow
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Crusts, Aggregates of Lath-like Crystals
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Sedimentary Sandstone Containing Uranium-vanadium Deposits
- Typical price
- $50-300 per specimen depending on size and rarity
Where rockhounds find vanalite
Classic worldwide localities
- Colorado Plateau, USA
- Montrose County, Colorado, USA
Field-hunting tip
Look in sedimentary sandstone containing uranium-vanadium deposits country — that is the host setting where vanalite typically forms. If you start seeing tyuyamunite, corvusite, gypsum in float, you are in the right ground. Field specimens usually show a crusts, aggregates of lath-like crystals habit, so train your eye for that shape before scanning the outcrop.




