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.

Hardness
~5
Mohs
Luster
Metallic to semimetallic
Streak
Ochre brown
Transparency
Opaque

Is this fetiasite?

5-step field check

Run through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.

  • 1
    Test the hardness
    Try to scratch fetiasite with a known reference. Fetiasite sits at Mohs ~5, softer than the next harder reference, harder than the previous one.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Streak: ochre brown.
  • 3
    Read the luster
    Hold the specimen under a strong light. Luster: metallic to semimetallic.
  • 4
    Match the color range
    Compare against the expected color range: brown, black.
  • 5
    Look at form & habit
    Crystal 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.

Common questions

How do you identify fetiasite?+
Mohs hardness is ~5. Luster: metallic to semimetallic. The streak is ochre brown. Common colors include brown, black.
Where is fetiasite found?+
Notable localities include East flank of Pizzo Cervandone, Alpe Devero, Val d’Aosta, Piedmont, Italy; Gorb, Binntal, Valais, Switzerland.
Is fetiasite safe to handle?+
Fetiasite contains arsenic and calls for real care. Contains arsenic, which is toxic; wash hands thoroughly after handling and do not inhale dust.
What rocks look like fetiasite?+
Fetiasite is most often confused with Ilmenite, Hematite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with fetiasite?+
Fetiasite commonly co-occurs with Asbecasite, Cafarsite, Cervandonite, Anatase, Chlorite, Feldspar. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does fetiasite form in?+
Where it forms: Deposited from arsenic-bearing solutions in Alpine fissures in gneisses of the upper greenschist to lower amphibolite facies. Working float back to the host body is the standard way to chase a fresh occurrence.
What is fetiasite used for?+
Fetiasite is used in collector.

Find fetiasite on the map

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