Vauxite is a rare phosphate mineral prized by collectors for its stunning sky-blue color and delicate radiating crystal sprays. It is almost exclusively found in the Siglo XX mine in Bolivia, where it forms in hydrothermal tin deposits.
Is this vauxite?
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 vauxite with a known reference. Vauxite sits at Mohs 3.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Vauxite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Vauxite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: sky blue, blue-green.
- 5Look at form & habitCrystal system: triclinic. Typical habit: radiating globular aggregates, crusts, or small prismatic crystals.
Often confused with
Vauxite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside vauxite
Minerals reported to co-occur with vauxite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Fe²⁺Al₂(PO₄)₂(OH)₂·6H₂O
- Mohs hardness
- 3.5
- Density
- 2.44 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Triclinic
- Crystal habit
- Radiating Globular Aggregates, Crusts, Or Small Prismatic Crystals
- Cleavage
- Perfect On {010}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Tin Veins in Altered Dacite Porphyry
- Typical price
- $50-500 depending on specimen size and clarity
Where rockhounds find vauxite
Classic worldwide localities
- Siglo XX Mine, Llallagua, Bolivia
Field-hunting tip
Look in hydrothermal tin veins in altered dacite porphyry country — that is the host setting where vauxite typically forms. If you start seeing paravauxite, metavauxite, childrenite in float, you are in the right ground. Field specimens usually show a radiating globular aggregates, crusts, or small prismatic crystals habit, so train your eye for that shape before scanning the outcrop.




