Belomarinaite is a rare potassium-sodium sulfate mineral typically found as a volcanic sublimate in fumaroles. It most commonly appears as small, colorless to white tabular crystals or thin crusts associated with other high-temperature volcanic minerals. It is highly soluble in water and requires careful storage in a humidity-controlled environment.
Is this belomarinaite?
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 belomarinaite with a known reference. Belomarinaite sits at Mohs 2-3, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Belomarinaite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Belomarinaite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, white.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: tabular crystals, crusts, or efflorescences.
Often confused with
Belomarinaite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside belomarinaite
Minerals reported to co-occur with belomarinaite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- NaKSO₄
- Mohs hardness
- 2-3
- Density
- 2.63 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Tabular Crystals, Crusts, Or Efflorescences
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Volcanic Fumaroles
- Typical price
- $50-300+ depending on matrix quality
Where rockhounds find belomarinaite
Classic worldwide localities
- Tolbachik volcano, Kamchatka, Russia
Field-hunting tip
Look in volcanic fumaroles country, the host setting where belomarinaite typically forms. If you start seeing aphthitalite, thenardite, sylvite in float, you are in the right ground. Field specimens usually show a tabular crystals, crusts, or efflorescences habit, so train your eye for that shape before scanning the outcrop.





