Pearceite is a silver arsenic sulfosalt often found as distinct, triangular or hexagonal tabular crystals in silver-rich hydrothermal deposits. It is frequently associated with other silver minerals and is highly sought after by systematic mineral collectors for its sharp crystal morphology and metallic luster.
Is this pearceite?
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 pearceite with a known reference. Pearceite 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. Pearceite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Pearceite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: black, dark gray.
- 5Look at form & habitCrystal system: trigonal. Typical habit: tabular hexagonal crystals, triangular prisms, massive.
Often confused with
Pearceite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside pearceite
Minerals reported to co-occur with pearceite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- [Ag₆As₂S₇][Ag₉CuS₄]
- Mohs hardness
- 3
- Density
- 6.1-6.3 g/cm³
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Trigonal
- Crystal habit
- Tabular Hexagonal Crystals, Triangular Prisms, Massive
- Cleavage
- None
- Rarity
- Uncommon
- Uses
- Collector, Ore Mineral
- Host rock
- Hydrothermal Silver-rich Veins
- Typical price
- $20-150 thumbnail, $200+ cabinet specimen
Where rockhounds find pearceite
Classic worldwide localities
- Montana, USA
- Chihuahua, Mexico
- Freiberg, Germany
- Jachymov, Czech Republic
Field-hunting tip
Look in hydrothermal silver-rich veins country — that is the host setting where pearceite typically forms. If you start seeing proustite, pyrargyrite, stephanite in float, you are in the right ground. Field specimens usually show a tabular hexagonal crystals, triangular prisms, massive habit, so train your eye for that shape before scanning the outcrop.







