Rossite is a rare vanadium mineral that typically forms as yellow, transparent to translucent crusts or small tabular crystals in oxidized zones of uranium-vanadium deposits. It is unstable in dry air and often dehydrates to form its dimorph, metarossite. Collectors should store this mineral in a sealed container to prevent it from crumbling into a powdery form.
Is this rossite?
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 rossite with a known reference. Rossite sits at Mohs 2-3, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: yellow.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous to somewhat pearly.
- 4Match the color rangeCompare against the expected color range: yellow.
- 5Look at form & habitCrystal system: triclinic. Typical habit: tabular crystals, crusts, efflorescences.
Often confused with
Rossite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside rossite
Minerals reported to co-occur with rossite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaV₂O₆·4H₂O
- Mohs hardness
- 2-3
- Density
- 2.45 g/cm³
- Colors
- Streak
- Yellow
- Luster
- Vitreous to somewhat pearly
- Transparency
- Transparent
- Crystal system
- Triclinic
- Crystal habit
- Tabular crystals, crusts, efflorescences
- Cleavage
- One direction, prominent
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In veinlets in carnotite-bearing sandstone (Bull Pen Canyon, Colorado, USA)
Where rockhounds find rossite
Classic worldwide localities
- Yellow Cat Wash, Thompsons district, Grand Co., Utah, USA
- Mesa No. 1 mine, Lukachukai Mountains, Arizona, USA
- Malargüe district, Mendoza Province, Argentina
Field-hunting tip
Where it forms: In veinlets in carnotite-bearing sandstone (Bull Pen Canyon, Colorado, USA). If you start seeing metarossite, carnotite, gypsum in float, you are in the right ground. Typical habit: tabular crystals, crusts, efflorescences. Train your eye for that shape before scanning the outcrop.







