Spryite is a rare silver arsenic sulfosalt that forms black equant crystals. It occurs in a hydrothermal Ag-Ge-Mn deposit. Associated minerals include proustite, argyrodite and galena. It was first described from Uchucchacua polymetallic deposit, Oyon district, Cajatambo, Lima Department, Peru.
Is this spryite?
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 spryite with a known reference. Spryite sits at Mohs 2.5-3, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Spryite leaves a pale yellow streak.
- 3Read the lusterHold the specimen under a strong light. Spryite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: black.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: equant crystals.
Often found alongside spryite
Minerals reported to co-occur with spryite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ag₈(As³⁺₀.₅As⁵⁺₀.₅)S₆
- Mohs hardness
- 2.5-3
- Density
- 6.334 g/cm³
- Colors
- Streak
- Pale Yellow
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Orthorhombic
- Crystal habit
- Equant Crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Polymetallic Deposits
Where rockhounds find spryite
Classic worldwide localities
- Uchucchacua polymetallic deposit, Lima Department, Peru
Field-hunting tip
Look in hydrothermal polymetallic deposits country, the host setting where spryite typically forms. If you start seeing galena, sphalerite, pyrite in float, you are in the right ground. Field specimens usually show a equant crystals habit, so train your eye for that shape before scanning the outcrop.




