Vihorlatite is a rare lead-bismuth telluride-sulfide mineral first identified in the Vihorlat Mountains of Slovakia. It typically occurs as small metallic grains or tabular crystals within epithermal vein systems associated with other bismuth minerals.
Is this vihorlatite?
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 vihorlatite with a known reference. Vihorlatite sits at Mohs 2.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Vihorlatite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Vihorlatite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: lead-gray, silver-white.
- 5Look at form & habitCrystal system: trigonal. Typical habit: tabular crystals, massive, granular.
Often confused with
Vihorlatite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside vihorlatite
Minerals reported to co-occur with vihorlatite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Bi₂Pb₄Te₇S₃
- Mohs hardness
- 2.5
- Density
- 7.35 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Trigonal
- Crystal habit
- Tabular Crystals, Massive, Granular
- Cleavage
- Perfect On {0001}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Epithermal Quartz-sulfide Veins
- Typical price
- $50-300 per specimen
Where rockhounds find vihorlatite
Classic worldwide localities
- Vihorlat Mountains, Slovakia
Field-hunting tip
Look in epithermal quartz-sulfide veins country — that is the host setting where vihorlatite typically forms. If you start seeing tetradymite, galena, gold in float, you are in the right ground. Field specimens usually show a tabular crystals, massive, granular habit, so train your eye for that shape before scanning the outcrop.



