Shchurovskyite is an exceptionally rare arsenate mineral found in the high-temperature fumaroles of the Tolbachik volcano in Russia. Collectors look for its characteristic greenish-yellow tabular crystals formed by volcanic gas deposition.
Is this shchurovskyite?
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 shchurovskyite with a known reference. Shchurovskyite 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: pale greenish.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: olive-green, dark olive-green, typically with a gray hue, olive drab.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals, incrustations, aggregates.
Often confused with
Shchurovskyite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside shchurovskyite
Minerals reported to co-occur with shchurovskyite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- K₂CaCu₆O₂(AsO₄)₄
- Mohs hardness
- 3
- Density
- 4.28 g/cm³
- Colors
- Streak
- Pale greenish
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular crystals, incrustations, aggregates
- Cleavage
- None
- 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 shchurovskyite
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 dmisokolovite, bradaczekite, tenorite in float, you are in the right ground. Typical habit: tabular crystals, incrustations, aggregates. Train your eye for that shape before scanning the outcrop.




