Argyrodite is a rare silver germanium sulfide primarily known for being the mineral in which the element germanium was first discovered. It typically occurs as opaque, metallic crystals in hydrothermal veins and is highly prized by collectors for its association with rare silver species.
Is this argyrodite?
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 argyrodite with a known reference. Argyrodite 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. Argyrodite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Argyrodite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: black, iron-black, steel-gray.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: short prismatic crystals, massive, reniform.
Often confused with
Argyrodite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside argyrodite
Minerals reported to co-occur with argyrodite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ag₈GeS₆
- Mohs hardness
- 2.5
- Density
- 6.2-6.3 g/cm³
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Orthorhombic
- Crystal habit
- Short Prismatic Crystals, Massive, Reniform
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector, Scientific Research
- Host rock
- Hydrothermal Silver-rich Veins
- Typical price
- $50-500 depending on specimen size and clarity
Where rockhounds find argyrodite
Classic worldwide localities
- Freiberg, Saxony, Germany
- Potosi, Bolivia
- Colquechaca, Bolivia
- Guanajuato, Mexico
Field-hunting tip
Look in hydrothermal silver-rich veins country — that is the host setting where argyrodite typically forms. If you start seeing canfieldite, acanthite, galena in float, you are in the right ground. Field specimens usually show a short prismatic crystals, massive, reniform habit, so train your eye for that shape before scanning the outcrop.






