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, 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.








