Cupropolybasite is a rare silver-copper sulfosalt member of the polybasite group that occurs in low-temperature hydrothermal veins. It is typically identified by its dark, metallic luster and its association with other silver-bearing minerals, often requiring X-ray diffraction or chemical analysis to distinguish definitively from other polybasite-group minerals.
Is this cupropolybasite?
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 cupropolybasite with a known reference. Cupropolybasite sits at Mohs 2.5-3 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Cupropolybasite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Cupropolybasite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: black, iron-black.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals, massive, granular.
Often confused with
Cupropolybasite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside cupropolybasite
Minerals reported to co-occur with cupropolybasite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Cu₁₆As₂Sb₂S₁₁
- Mohs hardness
- 2.5-3
- Density
- 6.39 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Monoclinic
- Crystal habit
- Tabular Crystals, Massive, Granular
- Cleavage
- Imperfect On {001}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Epithermal Hydrothermal Veins
- Typical price
- $20-150 thumbnail to cabinet
Where rockhounds find cupropolybasite
Classic worldwide localities
- Veta Rica mine, Mexico
- Guanajuato, Mexico
- Kongsberg, Norway
- Freiberg, Germany
Field-hunting tip
Look in epithermal hydrothermal veins country — that is the host setting where cupropolybasite typically forms. If you start seeing silver, acanthite, galena in float, you are in the right ground. Field specimens usually show a tabular crystals, massive, granular habit, so train your eye for that shape before scanning the outcrop.








