Tarkianite is an extremely rare copper-rhenium sulfide mineral found in hydrothermal ore deposits. It typically occurs as microscopic anhedral inclusions within other sulfide minerals, making it a difficult target for field collectors and usually requiring electron microprobe analysis for positive identification.
Is this tarkianite?
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 tarkianite with a known reference. Tarkianite sits at Mohs 3.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Tarkianite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Tarkianite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: steel-gray, white.
- 5Look at form & habitCrystal system: cubic. Typical habit: anhedral to subhedral grains.
Often confused with
Tarkianite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside tarkianite
Minerals reported to co-occur with tarkianite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Cu,Fe)₃(Re,Mo)₄S₈
- Mohs hardness
- 3.5
- Density
- 9.4-9.5 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Cubic
- Crystal habit
- Anhedral to Subhedral Grains
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Copper-molybdenum Deposits
- Typical price
- $100-500 per specimen
Where rockhounds find tarkianite
Classic worldwide localities
- Kadzharan copper-molybdenum deposit, Armenia
Field-hunting tip
Look in hydrothermal copper-molybdenum deposits country — that is the host setting where tarkianite typically forms. If you start seeing chalcopyrite, molybdenite, galena in float, you are in the right ground. Field specimens usually show a anhedral to subhedral grains habit, so train your eye for that shape before scanning the outcrop.





