Dmisokolovite is an extremely rare copper-aluminum arsenate mineral first discovered in the volcanic fumaroles of the Tolbachik volcano in Russia. It typically appears as small, bright emerald-green to light green, tabular crystals associated with other rare secondary volcanic minerals.
Is this dmisokolovite?
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 dmisokolovite with a known reference. Dmisokolovite sits at Mohs 3, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: light green.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: bright emerald-green, sometimes with a bluish hue.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals.
Often confused with
Dmisokolovite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside dmisokolovite
Minerals reported to co-occur with dmisokolovite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- K₃Cu₅AlO₂(AsO₄)₄
- Mohs hardness
- 3
- Density
- 4.26 g/cm³
- Colors
- Bright emerald-greenSometimes with a bluish hue
- Streak
- Light green
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular crystals
- Cleavage
- One imperfect direction
- Rarity
- Rare
- Uses
- Collector
- Host rock
- As sublimate incrustations and/or the product of reaction between rock and volcanic gas on the surface of basalt scoria in an active fumarole
Where rockhounds find dmisokolovite
Classic worldwide localities
- Arsenatnaya fumarole, Second scoria cone, Northern Breakthrough of the Great Tolbachik Fissure Eruption, Tolbachik volcano, Kamchatka Peninsula, Russia
Field-hunting tip
Where it forms: As sublimate incrustations and/or the product of reaction between rock and volcanic gas on the surface of basalt scoria in an active fumarole. If you start seeing shchurovskyite, bradaczekite, tenorite in float, you are in the right ground. Typical habit: tabular crystals. Train your eye for that shape before scanning the outcrop.




