Stephanite is a sought-after primary silver sulfide mineral prized by collectors for its sharp, complex pseudo-hexagonal crystal forms. It is typically found in hydrothermal veins associated with other silver-antimony sulfosalts and requires careful handling due to its brittle nature.
Is this stephanite?
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 stephanite with a known reference. Stephanite sits at Mohs 2-2.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Stephanite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Stephanite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: iron-black, lead-gray.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: tabular crystals, prismatic, often pseudo-hexagonal, massive.
Often confused with
Stephanite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside stephanite
Minerals reported to co-occur with stephanite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ag₅SbS₄
- Mohs hardness
- 2-2.5
- Density
- 6.2-6.3 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Orthorhombic
- Crystal habit
- Tabular Crystals, Prismatic, Often Pseudo-hexagonal, Massive
- Cleavage
- Imperfect
- Rarity
- Uncommon
- Uses
- Collector, Historical Silver Ore
- Host rock
- Epithermal Hydrothermal Silver Veins
- Typical price
- $20-200 per specimen depending on crystal quality and locality
Where rockhounds find stephanite
Classic worldwide localities
- Freiberg, Germany
- Příbram, Czech Republic
- Guanajuato, Mexico
- Chañarcillo, Chile
- Cobalt, Ontario, Canada
Field-hunting tip
Look in epithermal hydrothermal silver veins country — that is the host setting where stephanite typically forms. If you start seeing acanthite, pyrargyrite, proustite in float, you are in the right ground. Field specimens usually show a tabular crystals, prismatic, often pseudo-hexagonal, massive habit, so train your eye for that shape before scanning the outcrop.









