Hughesite is a rare hydrated sodium aluminum vanadate mineral that typically forms as small, bright yellow to greenish-yellow prismatic crystals. It is primarily found in the oxidized zones of vanadium-rich sandstone deposits, often occurring as crusts or tiny groupings within mine workings in the Colorado Plateau.
Is this hughesite?
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 hughesite with a known reference. Hughesite 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. Hughesite leaves a yellow streak.
- 3Read the lusterHold the specimen under a strong light. Hughesite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, greenish-yellow.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: prismatic to acicular crystals.
Often confused with
Hughesite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside hughesite
Minerals reported to co-occur with hughesite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₃Al₃(V₁₀O₂₈)·28H₂O
- Mohs hardness
- 2
- Density
- 2.42 g/cm³
- Colors
- Streak
- Yellow
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic to Acicular Crystals
- Cleavage
- Perfect in One Direction
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Vanadium-uranium Sandstone Deposits
- Typical price
- $50-300 thumbnail specimen
Where rockhounds find hughesite
Classic worldwide localities
- Burro Mine, Colorado, USA
- Hummer Mine, Colorado, USA
- Jo Dandy Mine, Colorado, USA
Field-hunting tip
Look in vanadium-uranium sandstone deposits country — that is the host setting where hughesite typically forms. If you start seeing pascoite, hewettite, rossite in float, you are in the right ground. Field specimens usually show a prismatic to acicular crystals habit, so train your eye for that shape before scanning the outcrop.



