Kuramite is a rare copper-tin sulfide mineral discovered in the Kurama Mountains. It typically occurs as small, metallic grains within hydrothermal ore deposits and is highly prized by advanced mineral collectors for its scarcity.
Is this kuramite?
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 kuramite with a known reference. Kuramite sits at Mohs 3.5-4 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Kuramite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Kuramite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: gray, blackish-gray.
- 5Look at form & habitCrystal system: tetragonal. Typical habit: massive, granular aggregates.
Often confused with
Kuramite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside kuramite
Minerals reported to co-occur with kuramite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Cu₃SnS₄
- Mohs hardness
- 3.5-4
- Density
- 4.56 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Tetragonal
- Crystal habit
- Massive, Granular Aggregates
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Sulfide Veins
- Typical price
- $50-300 per specimen
Where rockhounds find kuramite
Classic worldwide localities
- Kurama Mountains, Tajikistan
Field-hunting tip
Look in hydrothermal sulfide veins country — that is the host setting where kuramite typically forms. If you start seeing chalcopyrite, sphalerite, galena in float, you are in the right ground. Field specimens usually show a massive, granular aggregates habit, so train your eye for that shape before scanning the outcrop.






