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, 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.






