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. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 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
- Ca₃.₂[H₀.₆Si₂O₇](OH)
- Mohs hardness
- 5.5
- Density
- 2.94 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Platy crystals, granular aggregates
- Cleavage
- Perfect on {100}; poor on {010} and {001}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A secondary mineral in cavities and veins in hydrothermally altered and thermally metamorphosed limestones
Where rockhounds find killalaite
Classic worldwide localities
- Inishcrone, along the east shore of Killala Bay, Co. Sligo, and at Carneal, Co. Antrim, Ireland
- Güneyce-_ Ikizdere region, Trabzon Province, Turkey
Field-hunting tip
Where it forms: A secondary mineral in cavities and veins in hydrothermally altered and thermally metamorphosed limestones. If you start seeing calcite, afwillite, spurrite in float, you are in the right ground. Typical habit: platy crystals, granular aggregates. Train your eye for that shape before scanning the outcrop.





