Nekrasovite is a rare copper vanadium sulfosalt belonging to the tetrahedrite group. It typically occurs as small, metallic tetrahedral crystals within hydrothermal ore deposits and is highly prized by mineralogists for its scarcity and specific elemental composition.
Is this nekrasovite?
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 nekrasovite with a known reference. Nekrasovite sits at Mohs 4.5-5, 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: reddish brown.
- 5Look at form & habitCrystal system: cubic. Typical habit: granular.
Often confused with
Nekrasovite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside nekrasovite
Minerals reported to co-occur with nekrasovite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Cu₉Cu₄VSn₃S₁₆
- Mohs hardness
- 4.5-5
- Density
- 4.62 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Cubic
- Crystal habit
- Granular
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In ore aggregates within propylitic andesites and dacites (Khayragatsch deposit, Uzbekistan)
Where rockhounds find nekrasovite
Classic worldwide localities
- Campbell mine, Bisbee, Cochise Co., Arizona, USA
- Khayragatsch gold deposit, Chatkal-Kuramin Mountains, eastern Uzbekistan (type locality)
- Neves-Corvo, Portugal
- Persenk district, Rhodopes Mountains, Bulgaria
Field-hunting tip
Where it forms: In ore aggregates within propylitic andesites and dacites (Khayragatsch deposit, Uzbekistan). If you start seeing tetrahedrite–tennantite, luzonite–famatinite, pyrite in float, you are in the right ground. Typical habit: granular. Train your eye for that shape before scanning the outcrop.








