Teallite is a rare lead-tin sulfide mineral that typically forms as soft, flexible, gray-black platy crystals. It is most frequently found in hydrothermal vein deposits alongside other complex tin-bearing minerals like franckeite and cylindrite. Collectors value it for its metallic luster and its association with the unique mineral assemblages of the Bolivian tin-silver belt.
Is this teallite?
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 teallite with a known reference. Teallite sits at Mohs 1.5-2 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Teallite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Teallite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: black, lead-gray.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: tabular crystals, lamellar, foliated, or massive aggregates.
Often confused with
Teallite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside teallite
Minerals reported to co-occur with teallite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- PbSnS₂
- Mohs hardness
- 1.5-2
- Density
- 6.3-6.4 g/cm³
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Orthorhombic
- Crystal habit
- Tabular Crystals, Lamellar, Foliated, Or Massive Aggregates
- Cleavage
- Perfect Basal
- Rarity
- Rare
- Uses
- Collector, Scientific Research
- Host rock
- Hydrothermal Veins
- Typical price
- $20-150 thumbnail specimens
Where rockhounds find teallite
Classic worldwide localities
- Bolivia (Caracoles, Potosi)
- Russia (Primorsky Krai)
- Peru (Huancavelica)
Field-hunting tip
Look in hydrothermal veins country — that is the host setting where teallite typically forms. If you start seeing franckeite, cylindrite, galena in float, you are in the right ground. Field specimens usually show a tabular crystals, lamellar, foliated, or massive aggregates habit, so train your eye for that shape before scanning the outcrop.





