Tatarskite is an exceptionally rare hydrous calcium magnesium sulfate-carbonate-chloride mineral. It typically occurs as small, colorless to white tabular crystals within evaporite sequences and is primarily prized by advanced mineral collectors for its unique chemical composition.
Is this tatarskite?
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 tatarskite with a known reference. Tatarskite sits at Mohs 2.5, 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, pearly on cleavages.
- 4Match the color rangeCompare against the expected color range: colorless, light yellow.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: crystalline.
Often confused with
Tatarskite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside tatarskite
Minerals reported to co-occur with tatarskite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₆Mg₂(SO₄)₂(CO₃)₂(OH)₄Cl₄·7H₂O
- Mohs hardness
- 2.5
- Density
- 2.341 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous, pearly on cleavages
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Crystalline
- Cleavage
- Two sets of distinct pinacoidal cleavages
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A rare secondary mineral found in drill core in a marine salt deposit
Where rockhounds find tatarskite
Classic worldwide localities
- Chelkar salt dome, Ak-saı̆ Valley, Uralsk district, Kazakhstan
Field-hunting tip
Where it forms: A rare secondary mineral found in drill core in a marine salt deposit. If you start seeing anhydrite, halite, bischofite in float, you are in the right ground. Typical habit: crystalline. Train your eye for that shape before scanning the outcrop.







