Tacharanite is a rare calcium silicate mineral typically found as white, platy, or scaly aggregates within basalt cavities. It is often discovered in association with other zeolite-group minerals and calcium silicates in altered volcanic environments. Collectors prize it for its specific paragenesis within restricted geological sites like the Isle of Skye.
Is this tacharanite?
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 tacharanite with a known reference. Tacharanite sits at Mohs 3-4, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Tacharanite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Tacharanite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: white, colorless, pale yellow.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: platy aggregates, scaly masses.
Often confused with
Tacharanite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside tacharanite
Minerals reported to co-occur with tacharanite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₁₂Al₂Si₁₈O₅₇(OH)₁₀·~4H₂O
- Mohs hardness
- 3-4
- Density
- 2.45 g/cm³
- Streak
- White
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Platy Aggregates, Scaly Masses
- Cleavage
- Perfect in One Direction
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Basaltic Volcanic Rocks
- Typical price
- $20-100 per specimen
Where rockhounds find tacharanite
Classic worldwide localities
- Skye, Scotland
- Antrim, Northern Ireland
- Fuka, Japan
Field-hunting tip
Look in basaltic volcanic rocks country, the host setting where tacharanite typically forms. If you start seeing tobermorite, gyrolite, calcite in float, you are in the right ground. Field specimens usually show a platy aggregates, scaly masses habit, so train your eye for that shape before scanning the outcrop.




