Rakovanite is a rare hydrated sodium-vanadium polyoxometalate typically found as crusts or small tabular crystals in oxidation zones of vanadium-bearing sandstone deposits. Collectors should look for its distinctive deep red color within the clayey matrices of Colorado Plateau mines. Due to its solubility and sensitivity to hydration changes, it requires careful storage in a dry environment.
Is this rakovanite?
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 rakovanite with a known reference. Rakovanite 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. Rakovanite leaves a yellow-orange streak.
- 3Read the lusterHold the specimen under a strong light. Rakovanite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: dark red, reddish-brown.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals, crusts.
Often confused with
Rakovanite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside rakovanite
Minerals reported to co-occur with rakovanite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₃[H₃V₁₀O₂₈]·15H₂O
- Mohs hardness
- 2-3
- Density
- 2.4 g/cm³
- Colors
- Streak
- Yellow-orange
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular Crystals, Crusts
- Cleavage
- None Observed
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Sandstone Hosted Uranium-vanadium Deposits
- Typical price
- $50-300 per specimen
Where rockhounds find rakovanite
Classic worldwide localities
- Paradox Valley, Colorado, USA
- Montrose County, Colorado, USA
Field-hunting tip
Look in sandstone hosted uranium-vanadium deposits country — that is the host setting where rakovanite typically forms. If you start seeing pascoite, gypsum, carnotite in float, you are in the right ground. Field specimens usually show a tabular crystals, crusts habit, so train your eye for that shape before scanning the outcrop.




