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, 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.





