Borisenkoite is an extremely rare arsenate mineral discovered in the volcanic fumaroles of the Tolbachik volcano in Russia. It typically appears as dark green to black tabular crystals associated with other secondary copper and iron minerals in high-temperature volcanic environments.
Is this borisenkoite?
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 borisenkoite with a known reference. Borisenkoite sits at Mohs 4 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Borisenkoite leaves a light green streak.
- 3Read the lusterHold the specimen under a strong light. Borisenkoite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: dark green, black.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals.
Often confused with
Borisenkoite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside borisenkoite
Minerals reported to co-occur with borisenkoite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Cu₃Fe³⁺₂O₂(AsO₄)₂
- Mohs hardness
- 4
- Density
- 3.84 g/cm³
- Colors
- Streak
- Light Green
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular Crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Fumarolic Deposits
- Typical price
- n/a
Where rockhounds find borisenkoite
Classic worldwide localities
- Tolbachik volcano (Kamchatka, Russia)
Field-hunting tip
Look in fumarolic deposits country — that is the host setting where borisenkoite typically forms. If you start seeing lammerite, dolerophanite, tenorite in float, you are in the right ground. Field specimens usually show a tabular crystals habit, so train your eye for that shape before scanning the outcrop.



