Balyakinite is a rare copper tellurite mineral typically found as small, bright green platy crystals or thin crusts in oxidized ore zones. It is primarily sought by advanced mineral collectors specializing in tellurium species and is best identified by its distinct green color and association with other rare secondary tellurium minerals.
Is this balyakinite?
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 balyakinite with a known reference. Balyakinite 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. Streak: pale bluish green.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: blue green, gray green.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: platy crystals, crusts, aggregates.
Often confused with
Balyakinite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside balyakinite
Minerals reported to co-occur with balyakinite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CuTeO₃
- Mohs hardness
- 3.5
- Density
- 5.6 g/cm³
- Colors
- Streak
- Pale bluish green
- Luster
- Vitreous
- Transparency
- Semitransparent
- Crystal system
- Orthorhombic
- Crystal habit
- Platy crystals, crusts, aggregates
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A rare mineral formed in the oxidation zone as an alteration product of Cu–Te sulfides
Where rockhounds find balyakinite
Classic worldwide localities
- Pionersk deposit, eastern Sayan, and the Aginsk gold telluride deposit, Kamchatka, Far Eastern Region, Russia
Field-hunting tip
Where it forms: A rare mineral formed in the oxidation zone as an alteration product of Cu–Te sulfides. If you start seeing tetrahedrite, chalcopyrite, tellurite in float, you are in the right ground. Typical habit: platy crystals, crusts, aggregates. Train your eye for that shape before scanning the outcrop.






