Orthominasragrite is an extremely rare secondary vanadium sulfate mineral found primarily in the oxidized zone of vanadium deposits. It typically forms as delicate, light-blue crystalline crusts or aggregates that are highly sensitive to humidity and dehydration.
Is this orthominasragrite?
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 orthominasragrite with a known reference. Orthominasragrite sits at Mohs 2.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Orthominasragrite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Orthominasragrite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: blue, light blue.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: microcrystalline crusts, granular aggregates.
Often confused with
Orthominasragrite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside orthominasragrite
Minerals reported to co-occur with orthominasragrite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- VOSO₄·2H₂O
- Mohs hardness
- 2.5
- Density
- 2.12 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Microcrystalline Crusts, Granular Aggregates
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Vanadium Deposits
- Typical price
- $50-300 per thumbnail specimen
Where rockhounds find orthominasragrite
Classic worldwide localities
- Minasragra, Peru
Field-hunting tip
Look in oxidized vanadium deposits country — that is the host setting where orthominasragrite typically forms. If you start seeing pascoite, shoderite, gypsum in float, you are in the right ground. Field specimens usually show a microcrystalline crusts, granular aggregates habit, so train your eye for that shape before scanning the outcrop.




