Ambrinoite is a rare potassium arsenic antimony oxide, typically cinnabar-red. It occurs in an evaporite deposit probably formed by highly alkaline, low-temperature hydrothermal fluids. Associated minerals include sulfur, orpiment and gypsum. It was first described from the Cumbë Sûrdë quarry, Signols, Oulx, Upper Susa Valley, Torino, Piedmont, Italy.
Is this ambrinoite?
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 ambrinoite with a known reference. Ambrinoite 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: reddish.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous to resinous.
- 4Match the color rangeCompare against the expected color range: cinnabar-red.
- 5Look at form & habitCrystal system: triclinic. Typical habit: prismatic crystals.
Often confused with
Ambrinoite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside ambrinoite
Minerals reported to co-occur with ambrinoite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- [K,(NH₄)]₂(As,Sb)₆(Sb,As)₂S₁₃·H₂O
- Mohs hardness
- <2
- Density
- 3.276 g/cm³
- Colors
- Cinnabar-red
- Streak
- Reddish
- Luster
- Vitreous to resinous
- Transparency
- Transparent
- Crystal system
- Triclinic
- Crystal habit
- Prismatic crystals
- Cleavage
- Perfect on {001} and {010}, poor on {100}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In an evaporite deposit probably formed by highly alkaline, low-temperature hydrothermal fluids
Where rockhounds find ambrinoite
Classic worldwide localities
- Cumbë Sûrdë quarry, Signols, Oulx, Upper Susa Valley, Torino, Piedmont, Italy
Field-hunting tip
Where it forms: In an evaporite deposit probably formed by highly alkaline, low-temperature hydrothermal fluids. If you start seeing sulfur, orpiment, gypsum in float, you are in the right ground. Typical habit: prismatic crystals. Train your eye for that shape before scanning the outcrop.




