Hemusite is an extremely rare copper-tin-molybdenum sulfide mineral typically found in epithermal gold-copper deposits. It usually occurs as microscopic inclusions or fine-grained masses within other sulfide minerals, making hand-specimen identification difficult without laboratory analysis.
Is this hemusite?
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 hemusite with a known reference. Hemusite sits at Mohs 3.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Hemusite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Hemusite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: dark gray, black.
- 5Look at form & habitCrystal system: trigonal. Typical habit: massive, granular aggregates.
Often confused with
Hemusite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside hemusite
Minerals reported to co-occur with hemusite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Cu₆SnMoS₈
- Mohs hardness
- 3.5
- Density
- 6.32 g/cm³
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Trigonal
- Crystal habit
- Massive, Granular Aggregates
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Epithermal Deposits
- Typical price
- $50-300 per specimen
Where rockhounds find hemusite
Classic worldwide localities
- Chelopech deposit, Bulgaria
- Bor, Serbia
- Kidd Creek mine, Canada
Field-hunting tip
Look in hydrothermal epithermal deposits country — that is the host setting where hemusite typically forms. If you start seeing enargite, pyrite, luzonite 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.






