Korshunovskite is a rare magnesium chloride hydroxide mineral typically found as small, pearly-white lamellar crystals or thin plates. It is primarily identified within hydrothermal alteration zones in iron skarn deposits. Due to its solubility, it is best kept in a controlled, dry environment to prevent degradation.
Is this korshunovskite?
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 korshunovskite with a known reference. Korshunovskite 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. Korshunovskite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Korshunovskite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: white, colorless.
- 5Look at form & habitCrystal system: trigonal. Typical habit: lamellar crystals, thin plates, aggregates.
Often confused with
Korshunovskite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside korshunovskite
Minerals reported to co-occur with korshunovskite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Mg₂Cl(OH)₃·4H₂O
- Mohs hardness
- 2
- Density
- 2.05 g/cm³
- Streak
- White
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Trigonal
- Crystal habit
- Lamellar Crystals, Thin Plates, Aggregates
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Veins in Skarn Deposits
- Typical price
- $20-100 per specimen
Where rockhounds find korshunovskite
Classic worldwide localities
- Korshunovskoye iron deposit, Russia
- Kovdor Massif, Russia
Field-hunting tip
Look in hydrothermal veins in skarn deposits country — that is the host setting where korshunovskite typically forms. If you start seeing magnetite, serpentine, calcite in float, you are in the right ground. Field specimens usually show a lamellar crystals, thin plates, aggregates habit, so train your eye for that shape before scanning the outcrop.





