Cuboargyrite is a rare high-temperature polymorph of silver sulfide that typically occurs as cubic crystals. It is chemically identical to acanthite but crystallizes in the isometric system, often appearing as an inversion product. Collectors usually find it as small, metallic-gray crystals within complex silver-bearing hydrothermal vein systems.
Is this cuboargyrite?
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 cuboargyrite with a known reference. Cuboargyrite sits at Mohs 2.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Cuboargyrite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Cuboargyrite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: lead-gray, black.
- 5Look at form & habitCrystal system: cubic. Typical habit: pseudocubic crystals.
Often confused with
Cuboargyrite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside cuboargyrite
Minerals reported to co-occur with cuboargyrite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ag₂S
- Mohs hardness
- 2.5
- Density
- 7.3 g/cm³
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Cubic
- Crystal habit
- Pseudocubic Crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector, Scientific Research
- Host rock
- Hydrothermal Veins
- Typical price
- $50-500 depending on specimen quality and rarity
Where rockhounds find cuboargyrite
Classic worldwide localities
- Schneeberg, Germany
- Jáchymov, Czech Republic
- Guanajuato, Mexico
Field-hunting tip
Look in hydrothermal veins country — that is the host setting where cuboargyrite typically forms. If you start seeing native silver, proustite, pyrargyrite in float, you are in the right ground. Field specimens usually show a pseudocubic crystals habit, so train your eye for that shape before scanning the outcrop.






