Famatinite is a rare copper antimony sulfide often found as a massive or granular mineral in hydrothermal deposits. It is easily confused with its dimorph enargite, typically distinguished by a slightly redder metallic luster and distinct copper-red tint in reflected light.
Is this famatinite?
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 famatinite with a known reference. Famatinite 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. Famatinite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Famatinite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: copper-red, reddish-gray.
- 5Look at form & habitCrystal system: tetragonal. Typical habit: massive, granular, or crusts.
Often confused with
Famatinite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside famatinite
Minerals reported to co-occur with famatinite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Cu₃SbS₄
- Mohs hardness
- 3.5
- Density
- 4.57 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Tetragonal
- Crystal habit
- Massive, Granular, Or Crusts
- Cleavage
- Distinct On {112}
- Rarity
- Uncommon
- Uses
- Collector, Ore of Copper
- Host rock
- Epithermal Hydrothermal Veins
- Typical price
- $20-150 for thumbnail to cabinet specimens
Where rockhounds find famatinite
Classic worldwide localities
- Sierra de Famatina, Argentina
- Chuquicamata, Chile
- Lepanto mine, Philippines
- Bor, Serbia
Field-hunting tip
Look in epithermal hydrothermal veins country, the host setting where famatinite typically forms. If you start seeing enargite, pyrite, sphalerite in float, you are in the right ground. Field specimens usually show a massive, granular, or crusts habit, so train your eye for that shape before scanning the outcrop.







