Selenopolybasite is a rare selenium-dominant member of the polybasite group, typically found in low-temperature silver-rich hydrothermal veins. It usually appears as dark, metallic, pseudo-hexagonal tabular crystals that are difficult to distinguish visually from other members of the polybasite-pearceite series without laboratory analysis.
Is this selenopolybasite?
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 selenopolybasite with a known reference. Selenopolybasite sits at Mohs 3-3.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: black.
- 3Read the lusterHold the specimen under a strong light. Luster: metallic.
- 4Match the color rangeCompare against the expected color range: black.
- 5Look at form & habitCrystal system: trigonal. Typical habit: anhedral grains, microscopic crystals.
Often confused with
Selenopolybasite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside selenopolybasite
Minerals reported to co-occur with selenopolybasite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Cu(Ag,Cu)₆Ag₉Sb₂(S,Se)₉Se₂
- Mohs hardness
- 3-3.5
- Density
- 6.548 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Trigonal
- Crystal habit
- Anhedral grains, microscopic crystals
- Cleavage
- None detected
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In silicious veins through rhyolite porphyry altered at shallow depth by heated brines
Where rockhounds find selenopolybasite
Classic worldwide localities
- De Lamar mine, Owyhee County, Idaho, U.S.A (type locality)
Field-hunting tip
Where it forms: In silicious veins through rhyolite porphyry altered at shallow depth by heated brines. If you start seeing naumannite, covellite, pyrite in float, you are in the right ground. Typical habit: anhedral grains, microscopic crystals. Train your eye for that shape before scanning the outcrop.







