Canosioite is an extremely rare arsenate mineral that occurs as small, vibrant yellow to orange-yellow crystals. It is primarily found in hydrothermal veins associated with specific lead and iron-rich deposits in the Italian Alps. Due to its rarity and specific chemical composition, it is highly sought after by advanced systematic mineral collectors.
Is this canosioite?
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 canosioite with a known reference. Canosioite sits at Mohs 3.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Canosioite leaves a yellow streak.
- 3Read the lusterHold the specimen under a strong light. Canosioite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, yellowish-orange.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: tabular crystals, subparallel aggregates.
Often confused with
Canosioite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside canosioite
Minerals reported to co-occur with canosioite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pb₂Fe³⁺(AsO₄)₂(OH)
- Mohs hardness
- 3.5
- Density
- 4.57 g/cm³
- Colors
- Streak
- Yellow
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Tabular Crystals, Subparallel Aggregates
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Veins in Metamorphic Rocks
- Typical price
- $100-500+ for micro-specimens
Where rockhounds find canosioite
Classic worldwide localities
- Canosio, Piedmont, Italy
Field-hunting tip
Look in hydrothermal veins in metamorphic rocks country — that is the host setting where canosioite typically forms. If you start seeing quartz, goethite, beudantite in float, you are in the right ground. Field specimens usually show a tabular crystals, subparallel aggregates habit, so train your eye for that shape before scanning the outcrop.





