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, 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.






