Nabiasite is a very rare arsenate mineral originally discovered in the Pyrenees mountains of France. It typically occurs as small, sharp dodecahedral crystals in manganese-bearing mineral assemblages.
Is this nabiasite?
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 nabiasite with a known reference. Nabiasite sits at Mohs 5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: dark yellow, almost orange.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: dark red.
- 5Look at form & habitCrystal system: cubic. Typical habit: anhedral grains.
Often confused with
Nabiasite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside nabiasite
Minerals reported to co-occur with nabiasite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- BaMn₉(VO₄)₆(OH)₂
- Mohs hardness
- 5
- Density
- 4.307 g/cm³
- Colors
- Streak
- Dark yellow, almost orange
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Cubic
- Crystal habit
- Anhedral grains
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In an upper-greenschist-facies metamorphosed syn-sedimentary exhalative Mn deposit in radiolarian cherts along veinlets mineralized by hydrothermal remobilization
Where rockhounds find nabiasite
Classic worldwide localities
- Pla de Labasse deposit, near Nabias hamlet, Central Pyrenees, France
Field-hunting tip
Where it forms: In an upper-greenschist-facies metamorphosed syn-sedimentary exhalative Mn deposit in radiolarian cherts along veinlets mineralized by hydrothermal remobilization. If you start seeing rhodochrosite, barite, friedelite in float, you are in the right ground. Typical habit: anhedral grains. Train your eye for that shape before scanning the outcrop.





