Pintadoite is a rare vanadium mineral that typically occurs as thin, bright green crusts or efflorescences on sandstone surfaces. It is primarily found in the uranium-vanadium deposits of the Colorado Plateau, where it forms through the oxidation of primary vanadium-bearing minerals. Collectors should look for its distinctive yellow-green coating in desert sandstone outcrops.
Is this pintadoite?
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 pintadoite with a known reference. Pintadoite sits at Mohs 1-2, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: yellow green.
- 3Read the lusterHold the specimen under a strong light. Luster: dull.
- 4Match the color rangeCompare against the expected color range: light green, dark green.
- 5Look at form & habitCrystal system: tetragonal. Typical habit: efflorescences.
Often confused with
Pintadoite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside pintadoite
Minerals reported to co-occur with pintadoite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₂V₂O₇·9H₂O
- Mohs hardness
- 1-2
- Density
- 2.5 g/cm³
- Colors
- Streak
- Yellow green
- Luster
- Dull
- Transparency
- Semitransparent
- Crystal system
- Tetragonal
- Crystal habit
- Efflorescences
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- As an efflorescence on sandstone in protected outcrops
Where rockhounds find pintadoite
Classic worldwide localities
- Canyon Pintado, San Juan Co., New Mexico, USA (type locality)
Field-hunting tip
Where it forms: As an efflorescence on sandstone in protected outcrops. If you start seeing gypsum, quartz in float, you are in the right ground. Typical habit: efflorescences. Train your eye for that shape before scanning the outcrop.




