Killalaite is a rare calcium silicate mineral typically found in contact metamorphic limestone deposits. It is most frequently encountered as small, colorless platy crystals associated with calc-silicate skarns, making it a highly sought-after species for mineralogists and advanced collectors.
Is this killalaite?
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 killalaite with a known reference. Killalaite sits at Mohs 5.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Killalaite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Killalaite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, white.
- 5Look at form & habitCrystal system: trigonal. Typical habit: platy crystals, granular aggregates.
Often confused with
Killalaite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside killalaite
Minerals reported to co-occur with killalaite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₆Si₂O₇(OH)₂
- Mohs hardness
- 5.5
- Density
- 2.84 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Trigonal
- Crystal habit
- Platy Crystals, Granular Aggregates
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Metamorphosed Limestone (skarn Deposits)
- Typical price
- $50-300 per specimen depending on size and rarity
Where rockhounds find killalaite
Classic worldwide localities
- Killala Bay, Ireland
- Fuka, Japan
- Little Belt Mountains, Montana, USA
Field-hunting tip
Look in metamorphosed limestone (skarn deposits) country — that is the host setting where killalaite typically forms. If you start seeing calcite, cuspidine, wollastonite in float, you are in the right ground. Field specimens usually show a platy crystals, granular aggregates habit, so train your eye for that shape before scanning the outcrop.




