Atlasovite is an extremely rare copper-iron-bismuth oxychloride mineral discovered in the volcanic fumaroles of the Tolbachik volcano in Russia. It typically appears as dark, metallic-looking platy or tabular crystals formed by gas sublimation. Collectors prize it for its unique chemistry and extreme locality specificity.
Is this atlasovite?
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 atlasovite with a known reference. Atlasovite sits at Mohs 2-2.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: pale brown.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: dark brown.
- 5Look at form & habitCrystal system: tetragonal. Typical habit: platy crystals, tabular aggregates.
Often confused with
Atlasovite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside atlasovite
Minerals reported to co-occur with atlasovite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Cu₆FeBiO₄(SO₄)₅·KCl
- Mohs hardness
- 2-2.5
- Density
- 4.20 g/cm³
- Colors
- Streak
- Pale brown
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Tetragonal
- Crystal habit
- Platy crystals, tabular aggregates
- Cleavage
- On {001}, perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- As a volcanic sublimate
Where rockhounds find atlasovite
Classic worldwide localities
- Tolbachik fissure volcano, Kamchatka Peninsula, Russia
Field-hunting tip
Where it forms: As a volcanic sublimate. If you start seeing nabokoite, anglesite, dolerophanite in float, you are in the right ground. Typical habit: platy crystals, tabular aggregates. Train your eye for that shape before scanning the outcrop.





