Penzhinite is a rare silver-gold-copper sulfosalt mineral primarily identified from epithermal deposits in the Russian Far East. It typically occurs as microscopic anhedral grains intergrown with other precious metal minerals, requiring microscopic analysis for positive identification.
Is this penzhinite?
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 penzhinite with a known reference. Penzhinite 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: gray white, steel gray.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: anhedral grains.
Often confused with
Penzhinite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside penzhinite
Minerals reported to co-occur with penzhinite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Ag,Cu)₄Au(S,Se)₄
- Mohs hardness
- 2.5
- Density
- 8.35 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Hexagonal
- Crystal habit
- Anhedral grains
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector, Scientific research
- Host rock
- In a near-surface Au–Ag deposit
Where rockhounds find penzhinite
Classic worldwide localities
- Sergeevskoye Au–Ag deposit, 60 km northeast of Pevirechenskii, near the Penzhina River, northern Kamchatka, Russia (type locality)
Field-hunting tip
Where it forms: In a near-surface Au–Ag deposit. If you start seeing gold, aguilarite, chalcopyrite in float, you are in the right ground. Typical habit: anhedral grains. Train your eye for that shape before scanning the outcrop.





