Cafarsite is a rare calcium-titanium-iron arsenite mineral known almost exclusively from the Binn Valley of Switzerland. It typically appears as dark, complex dodecahedral crystals embedded in dolomite marble and is highly prized by advanced mineral collectors for its unique chemistry and crystallography.
Is this cafarsite?
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 cafarsite with a known reference. Cafarsite sits at Mohs 5.5-6, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: yellow-brown.
- 3Read the lusterHold the specimen under a strong light. Luster: submetallic.
- 4Match the color rangeCompare against the expected color range: dark brown, brownish yellow, brownish black, dark red.
- 5Look at form & habitCrystal system: cubic. Typical habit: dodecahedral crystals.
Often confused with
Cafarsite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside cafarsite
Minerals reported to co-occur with cafarsite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Ca,Na,□)₁₉Ti₈Fe₄Fe₄(AsO₃)₂₈F
- Mohs hardness
- 5.5-6
- Density
- 3.90 g/cm³
- Streak
- Yellow-brown
- Luster
- Submetallic
- Transparency
- Opaque to translucent in thin fragments
- Crystal system
- Cubic
- Crystal habit
- Dodecahedral crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- On cleft faces in orthogneiss (Cherbadung, Switzerland)
Where rockhounds find cafarsite
Classic worldwide localities
- East flank of Pizzo Cervandone, Alpe Devero, Val d’Aosta, Piedmont, Italy
- Hemlo gold mine, Ontario, Canada
Field-hunting tip
Where it forms: On cleft faces in orthogneiss (Cherbadung, Switzerland). If you start seeing asbecasite, gasparite-, chernovite in float, you are in the right ground. Typical habit: dodecahedral crystals. Train your eye for that shape before scanning the outcrop.


