Saranchinaite is a very rare copper sulfate mineral discovered in the volcanic fumaroles of the Tolbachik volcano. It typically occurs as small, light-blue to nearly white tabular crystals formed through high-temperature volcanic gas sublimation.
Is this saranchinaite?
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 saranchinaite with a known reference. Saranchinaite sits at Mohs 2, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: nearly white, sky-blue.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals.
Often confused with
Saranchinaite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside saranchinaite
Minerals reported to co-occur with saranchinaite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₂Cu(SO₄)₂
- Mohs hardness
- 2
- Density
- 2.937 g/cm³
- Colors
- Nearly whiteSky-blue
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent to translucent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A sublimate from volcanic gases with temperature ~600 °C at a fumarole
Where rockhounds find saranchinaite
Classic worldwide localities
- Saranchinaitovaya fumarole, Naboko Scoria cone, Tolbachik volcano, Kamchatka, Far-Eastern Region, Russia
Field-hunting tip
Where it forms: A sublimate from volcanic gases with temperature ~600 °C at a fumarole. If you start seeing euchlorine, anhydrite, itelmenite in float, you are in the right ground. Typical habit: tabular crystals. Train your eye for that shape before scanning the outcrop.




