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. Delrioite leaves a yellow streak.
- 3Read the lusterHold the specimen under a strong light. Delrioite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, yellowish-green.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular, radiating clusters, crusts.
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
- CaSrV₂O₆(OH)₂·3H₂O
- Mohs hardness
- 2
- Density
- 2.8 g/cm³
- Colors
- Streak
- Yellow
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular, Radiating Clusters, Crusts
- Cleavage
- Distinct On {001}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Vanadium-uranium-bearing Sedimentary Rocks
- Typical price
- $50-300 per thumbnail specimen
Where rockhounds find delrioite
Classic worldwide localities
- Colorado Plateau, USA
- Paradox Valley, Colorado
- Montrose County, Colorado
Field-hunting tip
Look in vanadium-uranium-bearing sedimentary rocks country — that is the host setting where delrioite typically forms. If you start seeing pascoite, carnotite, rossite in float, you are in the right ground. Field specimens usually show a tabular, radiating clusters, crusts habit, so train your eye for that shape before scanning the outcrop.





