Naumannite is a rare silver selenide mineral typically found in low-temperature hydrothermal veins. It is distinguished by its heavy feel, metallic lead-gray color, and characteristic association with other rare selenides and precious metals.
Is this naumannite?
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 naumannite with a known reference. Naumannite 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. Streak: black.
- 3Read the lusterHold the specimen under a strong light. Luster: metallic.
- 4Match the color rangeCompare against the expected color range: grayish black, iron black.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: massive.
Often confused with
Naumannite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside naumannite
Minerals reported to co-occur with naumannite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ag₂Se
- Mohs hardness
- 2.5
- Density
- 7.0-8.0 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Orthorhombic
- Crystal habit
- Massive
- Cleavage
- Perfect
- Rarity
- Uncommon
- Uses
- Collector, Ore of silver
- Host rock
- In hydrothermal veins deficient in sulfur, associated with other selenides, quartz, and carbonates
Where rockhounds find naumannite
Classic worldwide localities
- Republic, Ferry Co., and in the L-D mine, Wenatchee, Chelan Co., Washington, USA
- De Lamar mine, Silver City district, Owyhee Co., and from the 4th of July mine, Yankee Fork, Custer Co., Idaho, USA
- Ken Snyder mine, Gold Circle district, Elko Co., and at the Rex Grande deposit, Midas, Elko Co., Nevada, USA
- Harz Mountains, at Tilkerode (type locality) and St. Andreasberg, Germany
- Săcărı̂mb (Nagyág), Romania
- Předbořice deposit, Czech Republic
Field-hunting tip
Where it forms: In hydrothermal veins deficient in sulfur, associated with other selenides, quartz, and carbonates. If you start seeing clausthalite, aguilarite, acanthite in float, you are in the right ground. Typical habit: massive. Train your eye for that shape before scanning the outcrop.








