Ciriottiite is a rare sulfosalt mineral primarily found in manganese-rich hydrothermal deposits in Italy. It typically occurs as small, dark brown to black anhedral grains associated with manganese oxides and various sulfides. Due to its extreme rarity and very small grain size, it is almost exclusively sought after by advanced systematic mineral collectors.
Is this ciriottiite?
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 ciriottiite with a known reference. Ciriottiite 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. Ciriottiite leaves a brown streak.
- 3Read the lusterHold the specimen under a strong light. Ciriottiite typically shows a submetallic luster.
- 4Match the color rangeCompare against the expected color range: dark brown, black.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: anhedral to subhedral grains.
Often confused with
Ciriottiite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside ciriottiite
Minerals reported to co-occur with ciriottiite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₂CuFe₂As₄S₁₀
- Mohs hardness
- 3.5
- Density
- 4.55 g/cm³
- Colors
- Streak
- Brown
- Luster
- Submetallic
- Transparency
- Opaque
- Crystal system
- Monoclinic
- Crystal habit
- Anhedral to Subhedral Grains
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Manganese Ore Deposits
- Typical price
- $100-500 depending on specimen quality
Where rockhounds find ciriottiite
Classic worldwide localities
- Monte Nero, Val Graveglia, Liguria, Italy
Field-hunting tip
Look in hydrothermal manganese ore deposits country — that is the host setting where ciriottiite typically forms. If you start seeing braunite, quartz, calcite in float, you are in the right ground. Field specimens usually show a anhedral to subhedral grains habit, so train your eye for that shape before scanning the outcrop.





