Belakovskiite is a rare sulfate-selenate mineral discovered in the oxidized zones of burning coal dumps in the Chelyabinsk coal basin of Russia. It typically occurs as small, delicate, pale yellow tabular crystals formed by complex chemical reactions in anthropogenic settings. Due to its extreme rarity and specific formation conditions, it is highly sought after by advanced systematic mineral collectors.
Is this belakovskiite?
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 belakovskiite with a known reference. Belakovskiite 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. Belakovskiite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Belakovskiite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, pale yellow.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals.
Often confused with
Belakovskiite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside belakovskiite
Minerals reported to co-occur with belakovskiite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₂Ca(SO₄)(SeO₄)·H₂O
- Mohs hardness
- 2
- Density
- 2.88 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular Crystals
- Cleavage
- Perfect On {010}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Zones of Coal Mine Fires
- Typical price
- $100-500+ per specimen
Where rockhounds find belakovskiite
Classic worldwide localities
- Chelyabinsk Oblast, Russia
Field-hunting tip
Look in oxidized zones of coal mine fires country — that is the host setting where belakovskiite typically forms. If you start seeing gypsum, jarosite, halite in float, you are in the right ground. Field specimens usually show a tabular crystals habit, so train your eye for that shape before scanning the outcrop.




