Cairncrossite is a rare strontium-calcium silicate that typically forms as delicate, pearly-white radiating aggregates. It is primarily found within the manganese-rich environments of the Kalahari Manganese Field, often appearing as distinct micro-crystals associated with other rare hydrothermal minerals.
Is this cairncrossite?
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 cairncrossite with a known reference. Cairncrossite sits at Mohs 3 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Cairncrossite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Cairncrossite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: white, colorless.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: platy crystals, radial aggregates.
Often confused with
Cairncrossite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside cairncrossite
Minerals reported to co-occur with cairncrossite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Sr,Ca)₁₄(Si₄O₁₀)₂(Si₂O₇)(OH)₄·~20H₂O
- Mohs hardness
- 3
- Density
- 2.16 g/cm³
- Streak
- White
- Luster
- Pearly
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Platy Crystals, Radial Aggregates
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Veins in Manganese Ore Deposits
- Typical price
- $50-300 per specimen
Where rockhounds find cairncrossite
Classic worldwide localities
- Kalahari Manganese Field, South Africa
Field-hunting tip
Look in hydrothermal veins in manganese ore deposits country — that is the host setting where cairncrossite typically forms. If you start seeing manganite, hausmannite, calcite in float, you are in the right ground. Field specimens usually show a platy crystals, radial aggregates habit, so train your eye for that shape before scanning the outcrop.







