Rhodostannite is an uncommon copper iron tin sulfide typically found in hydrothermal tin deposits. It is often indistinguishable from stannite without professional X-ray diffraction or chemical analysis and typically occurs as metallic, dark-colored grains or massive aggregates.
Is this rhodostannite?
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 rhodostannite with a known reference. Rhodostannite sits at Mohs 4 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Rhodostannite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Rhodostannite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: black, gray.
- 5Look at form & habitCrystal system: tetragonal. Typical habit: massive, granular, rarely tabular crystals.
Often confused with
Rhodostannite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside rhodostannite
Minerals reported to co-occur with rhodostannite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Cu₂FeSn₃S₈
- Mohs hardness
- 4
- Density
- 4.49 g/cm³
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Tetragonal
- Crystal habit
- Massive, Granular, Rarely Tabular Crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector, Scientific Research
- Host rock
- Hydrothermal Tin-bearing Veins
- Typical price
- $50-300 per specimen depending on size and association
Where rockhounds find rhodostannite
Classic worldwide localities
- Llallagua, Bolivia
- Oruro, Bolivia
- Pirquitas, Argentina
Field-hunting tip
Look in hydrothermal tin-bearing veins country — that is the host setting where rhodostannite typically forms. If you start seeing stannite, cassiterite, pyrrhotite in float, you are in the right ground. Field specimens usually show a massive, granular, rarely tabular crystals habit, so train your eye for that shape before scanning the outcrop.




