Cupropearceite is a rare copper-dominant member of the pearceite group, appearing as dark, metallic hexagonal plates or massive aggregates. It is typically found in low-to-medium temperature hydrothermal sulfide deposits and requires chemical analysis or X-ray diffraction to reliably distinguish from other members of the tennantite-pearceite series.
Is this cupropearceite?
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 cupropearceite with a known reference. Cupropearceite sits at Mohs 3, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Cupropearceite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Cupropearceite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: black, iron-black.
- 5Look at form & habitCrystal system: trigonal. Typical habit: tabular crystals, hexagonal plates, massive.
Often confused with
Cupropearceite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside cupropearceite
Minerals reported to co-occur with cupropearceite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Cu,Ag)₁₆As₂S₁₁
- Mohs hardness
- 3
- Density
- 6.2 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Trigonal
- Crystal habit
- Tabular Crystals, Hexagonal Plates, Massive
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Veins in Sedimentary and Metamorphic Rocks
- Typical price
- $50-300 per specimen
Where rockhounds find cupropearceite
Classic worldwide localities
- Dzhezkazgan, Kazakhstan
- Rudabanya, Hungary
- Guanajuato, Mexico
Field-hunting tip
Look in hydrothermal veins in sedimentary and metamorphic rocks country, the host setting where cupropearceite typically forms. If you start seeing tennantite, galena, sphalerite in float, you are in the right ground. Field specimens usually show a tabular crystals, hexagonal plates, massive habit, so train your eye for that shape before scanning the outcrop.






