Popovite is a rare copper arsenate mineral found in the high-temperature volcanic fumaroles of the Tolbachik volcano. It typically appears as tiny, colorless to pale yellow tabular crystals formed through volcanic gas deposition. Due to its toxicity and extreme rarity, it is sought almost exclusively by advanced micromount collectors.
Is this popovite?
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 popovite with a known reference. Popovite 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: light olive-green to light yellow-green.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous to greasy.
- 4Match the color rangeCompare against the expected color range: olive-green, dark olive-green.
- 5Look at form & habitCrystal system: triclinic. Typical habit: tabular crystals, crusts.
Often confused with
Popovite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside popovite
Minerals reported to co-occur with popovite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Cu₅O₂(AsO₄)₂
- Mohs hardness
- ~3.5
- Density
- 5.30 g/cm³
- Streak
- Light olive-green to light yellow-green
- Luster
- Vitreous to greasy
- Transparency
- Transparent
- Crystal system
- Triclinic
- Crystal habit
- Tabular crystals, crusts
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Formed as sublimates on basaltic scoria around an active volcanic fumarole
Where rockhounds find popovite
Classic worldwide localities
- Arsenatnaya fumarole, Second scoria cone of the Northern Breakthrough of the Great Tolbachik Fissure Eruption, Tolbachik volcano, Kamchatka, Russia
Field-hunting tip
Where it forms: Formed as sublimates on basaltic scoria around an active volcanic fumarole. If you start seeing ericlaxmanite, kozyrevskite, urusovite in float, you are in the right ground. Typical habit: tabular crystals, crusts. Train your eye for that shape before scanning the outcrop.



