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, 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.









