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 ~1, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: pale blue.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: bright blue, pale blue.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: encrustations.
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
- VO(SO₄)(H₂O)₅
- Mohs hardness
- ~1
- Density
- 2.00 g/cm³
- Colors
- Streak
- Pale blue
- Luster
- Vitreous
- Transparency
- Semitransparent
- Crystal system
- Orthorhombic
- Crystal habit
- Encrustations
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In a silicified tree, formed as an oxidation product of pyrite reacting with vanadium-rich organic material
Where rockhounds find orthominasragrite
Classic worldwide localities
- Triassic Shinarump conglomerate at the North Mesa Mina group, Emery County, Utah, USA (type locality)
Field-hunting tip
Where it forms: In a silicified tree, formed as an oxidation product of pyrite reacting with vanadium-rich organic material. If you start seeing minasragrite, pyrite, szomolnokite in float, you are in the right ground. Typical habit: encrustations. Train your eye for that shape before scanning the outcrop.






