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, 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.





