Viaeneite is a rare iron-lead sulfide-oxide mineral that occurs as black, microcrystalline crusts. It was discovered in the Engis zinc-lead deposit in Belgium, typically forming in association with other sulfide minerals in limestone.
Is this viaeneite?
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 viaeneite with a known reference. Viaeneite sits at Mohs 3, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: black.
- 3Read the lusterHold the specimen under a strong light. Luster: metallic.
- 4Match the color rangeCompare against the expected color range: yellow.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: aggregates, spherical.
Often confused with
Viaeneite vs. its common look-alikes, and how to tell them apart in the field.

How to tell apart: Pyrite is the harder of the two (Mohs 6-6.5 vs. 3); streak differs, so Viaeneite leaves black, Pyrite leaves greenish black to brownish black.

How to tell apart: Marcasite is the harder of the two (Mohs 6-6.5 vs. 3); streak differs, so Viaeneite leaves black, Marcasite leaves grayish or brownish black.
Often found alongside viaeneite
Minerals reported to co-occur with viaeneite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Fe,Pb)₄S₈O
- Mohs hardness
- 3
- Density
- 3.8 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Monoclinic
- Crystal habit
- Aggregates, spherical
- Cleavage
- On {110}, clearly observed under transmission electron microscopy
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In a carbonate-hosted Pb–Zn deposit
Where rockhounds find viaeneite
Classic worldwide localities
- Mallieue Pb–Zn deposit, Engis, about 40 km southwest of Liège, Belgium (type locality)
Field-hunting tip
Where it forms: In a carbonate-hosted Pb–Zn deposit. If you start seeing pyrite, melnikovite, marcasite in float, you are in the right ground. Typical habit: aggregates, spherical. Train your eye for that shape before scanning the outcrop.




