Franckeite is a complex lead-tin sulfide mineral often found in distinctive thin, flexible, tabular, or fan-shaped crystals. It is primarily sourced from tin-bearing hydrothermal deposits in Bolivia and is highly prized by collectors for its unique layered crystal structure.
Is this franckeite?
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 franckeite with a known reference. Franckeite sits at Mohs 2.5-3 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Franckeite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Franckeite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: black, dark gray.
- 5Look at form & habitCrystal system: triclinic. Typical habit: tabular crystals, foliated masses, radiating aggregates.
Often confused with
Franckeite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside franckeite
Minerals reported to co-occur with franckeite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Pb,Sn)₆FeSn₂S₁₄
- Mohs hardness
- 2.5-3
- Density
- 5.5-5.9 g/cm³
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Triclinic
- Crystal habit
- Tabular Crystals, Foliated Masses, Radiating Aggregates
- Cleavage
- Perfect Basal
- Rarity
- Rare
- Uses
- Collector, Geological Study
- Host rock
- Hydrothermal Veins
- Typical price
- $20-150 for thumbnail to small cabinet specimens
Where rockhounds find franckeite
Classic worldwide localities
- Chocaya, Bolivia
- Tasna, Bolivia
- Oruro, Bolivia
- San Jose Mine, Bolivia
Field-hunting tip
Look in hydrothermal veins country — that is the host setting where franckeite typically forms. If you start seeing cylindrite, cassiterite, wurtzite in float, you are in the right ground. Field specimens usually show a tabular crystals, foliated masses, radiating aggregates habit, so train your eye for that shape before scanning the outcrop.






