Ilinskite is a rare volcanic mineral found exclusively in the fumaroles of the Tolbachik volcano in Russia. It typically appears as distinct, bright yellow to orange tabular crystals or crusts that form in high-temperature volcanic environments.
Is this ilinskite?
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 ilinskite with a known reference. Ilinskite 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. Ilinskite leaves a yellow streak.
- 3Read the lusterHold the specimen under a strong light. Ilinskite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, orange, brown.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: tabular crystals, crusts, aggregates.
Often confused with
Ilinskite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside ilinskite
Minerals reported to co-occur with ilinskite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- NaCu₅O₂(SeO₃)₂Cl₃
- Mohs hardness
- 3
- Density
- 3.31 g/cm³
- Streak
- Yellow
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Tabular Crystals, Crusts, Aggregates
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Fumarole Deposits
- Typical price
- $100-500+ for thumbnail specimens
Where rockhounds find ilinskite
Classic worldwide localities
- Tolbachik volcano, Kamchatka, Russia
Field-hunting tip
Look in fumarole deposits country — that is the host setting where ilinskite typically forms. If you start seeing sophiite, burnsite, tenorite in float, you are in the right ground. Field specimens usually show a tabular crystals, crusts, aggregates habit, so train your eye for that shape before scanning the outcrop.


