Fetiasite is an extremely rare arsenic-bearing mineral known primarily from the type locality in the Aosta Valley, Italy. It typically forms small, dark, submetallic tabular crystals embedded within manganese-rich metamorphic rocks.
Is this fetiasite?
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 fetiasite with a known reference. Fetiasite sits at Mohs ~5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: ochre brown.
- 3Read the lusterHold the specimen under a strong light. Luster: metallic to semimetallic.
- 4Match the color rangeCompare against the expected color range: brown, black.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: crystalline, globular, tabular.
Often confused with
Fetiasite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside fetiasite
Minerals reported to co-occur with fetiasite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Fe²⁺,Fe³⁺,Ti)₃(As³⁺O₃)₄
- Mohs hardness
- ~5
- Density
- 4.6 g/cm³
- Streak
- Ochre brown
- Luster
- Metallic to semimetallic
- Transparency
- Opaque
- Crystal system
- Monoclinic
- Crystal habit
- Crystalline, globular, tabular
- Cleavage
- {100}, perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Deposited from arsenic-bearing solutions in Alpine fissures in gneisses of the upper greenschist to lower amphibolite facies
Where rockhounds find fetiasite
Classic worldwide localities
- East flank of Pizzo Cervandone, Alpe Devero, Val d’Aosta, Piedmont, Italy
- Gorb, Binntal, Valais, Switzerland
Field-hunting tip
Where it forms: Deposited from arsenic-bearing solutions in Alpine fissures in gneisses of the upper greenschist to lower amphibolite facies. If you start seeing asbecasite, cafarsite, cervandonite in float, you are in the right ground. Typical habit: crystalline, globular, tabular. Train your eye for that shape before scanning the outcrop.








