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 — that is 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.







