Cuproneyite is a rare copper-lead-bismuth selenide mineral known for its dark, metallic luster and occurrence in seleniferous hydrothermal deposits. It is typically found in massive forms or as microscopic inclusions within other sulfide minerals, making it a challenging mineral for general collectors to identify without analytical testing.
Is this cuproneyite?
4-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 cuproneyite with a known reference. Cuproneyite sits at Mohs ~3, softer than the next harder reference, harder than the previous one.
- 2Read the lusterHold the specimen under a strong light. Luster: metallic.
- 3Match the color rangeCompare against the expected color range: silver-gray.
- 4Look at form & habitCrystal system: monoclinic. Typical habit: massive, crusts, acicular.
Often confused with
Cuproneyite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside cuproneyite
Minerals reported to co-occur with cuproneyite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Cu₇Pb₂₇Bi₂₅S₆₈
- Mohs hardness
- ~3
- Density
- 7.113 g/cm³
- Colors
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Monoclinic
- Crystal habit
- Massive, crusts, acicular
- Cleavage
- Perfect along [001]
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In diopside skarn hosting polymetallic mineralization related to contact metamorphism
Where rockhounds find cuproneyite
Classic worldwide localities
- Băiţa Bihor, Romania
Field-hunting tip
Where it forms: In diopside skarn hosting polymetallic mineralization related to contact metamorphism. If you start seeing cosalite, hammarite-friedrichite, calcite in float, you are in the right ground. Typical habit: massive, crusts, acicular. Train your eye for that shape before scanning the outcrop.





