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: monoclinic. 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
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Platy Crystals, Granular Aggregates
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Metamorphosed Limestone (skarn Deposits)
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, 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.




