Delrioite is a rare hydrated calcium strontium vanadate found primarily in the oxidized zones of vanadium-uranium deposits. It typically forms as delicate, transparent yellow tabular crystals or crusts coating sandstone surfaces. Due to its scarcity and fragility, it is highly sought after by advanced collectors of secondary vanadium minerals.
Is this delrioite?
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 delrioite with a known reference. Delrioite 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. Streak: pale yellow green.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous to pearly.
- 4Match the color rangeCompare against the expected color range: yellow brown, light yellow green, dark green.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: acicular, aggregates, radial.
Often confused with
Delrioite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside delrioite
Minerals reported to co-occur with delrioite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Sr(VO₃)₂·4H₂O
- Mohs hardness
- ~2
- Density
- 3.1 g/cm³
- Colors
- Streak
- Pale yellow green
- Luster
- Vitreous to pearly
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Acicular, aggregates, radial
- Cleavage
- Distinct on {001}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- An efflorescence on sandstone of the Salt Wash member of the Jurassic Morrison Formation associated with a U–V deposit
Where rockhounds find delrioite
Classic worldwide localities
- Jo Dandy mine, Montrose County, Colorado, USA (type locality)
Field-hunting tip
Where it forms: An efflorescence on sandstone of the Salt Wash member of the Jurassic Morrison Formation associated with a U–V deposit. If you start seeing metadelrioite, rossite, metarossite in float, you are in the right ground. Typical habit: acicular, aggregates, radial. Train your eye for that shape before scanning the outcrop.





