Saneroite is a rare manganese silicate mineral typically identified by its vibrant orange, fibrous, or radiating needle-like crystal clusters. It is highly sought after by collectors for its limited locality occurrences, most notably in the manganese mines of the Val Graveglia region in Italy.
Is this saneroite?
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 saneroite with a known reference. Saneroite sits at Mohs 6-7, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: resinous to greasy.
- 4Match the color rangeCompare against the expected color range: light orange.
- 5Look at form & habitCrystal system: triclinic. Typical habit: aggregates, tabular.
Often confused with
Saneroite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside saneroite
Minerals reported to co-occur with saneroite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- NaMn₅[Si₅O₁₄(OH)](VO₃)(OH)
- Mohs hardness
- 6-7
- Density
- 3.47 g/cm³
- Colors
- Streak
- White
- Luster
- Resinous to greasy
- Transparency
- Transparent to translucent
- Crystal system
- Triclinic
- Crystal habit
- Aggregates, tabular
- Cleavage
- Perfect in two perpendicular directions
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In veins in manganese ores associated with low-grade prehnite-pumpellyite facies metamorphic recrystallization of siliceous-hematitic sediments (Val Graveglia, Italy)
Where rockhounds find saneroite
Classic worldwide localities
- Gambatesa and Molinello manganese mines, near Chiavari, Val Graveglia, Liguria, Italy
- Fianel mine, Val Ferrera, Graubünden, Switzerland
Field-hunting tip
Where it forms: In veins in manganese ores associated with low-grade prehnite-pumpellyite facies metamorphic recrystallization of siliceous-hematitic sediments (Val Graveglia, Italy). If you start seeing quartz, barite, caryopilite in float, you are in the right ground. Typical habit: aggregates, tabular. Train your eye for that shape before scanning the outcrop.






