Hillebrandite is a rare calcium silicate hydrate typically found as a result of contact metamorphism in limestone or as a hydration product of calcium silicates. It most commonly occurs in fibrous or massive aggregates and is noted for its association with other rare calcium-rich minerals in skarn deposits.
Is this hillebrandite?
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 hillebrandite with a known reference. Hillebrandite sits at Mohs 5-6, 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: white, colorless, greenish white.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: fibrous, radial.
Often confused with
Hillebrandite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside hillebrandite
Minerals reported to co-occur with hillebrandite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₂SiO₃(OH)₂
- Mohs hardness
- 5-6
- Density
- 2.66-2.69 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent to translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Fibrous, radial
- Cleavage
- {010}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In limestone affected by high-grade contact metamorphism
Where rockhounds find hillebrandite
Classic worldwide localities
- Crestmore, Riverside Co., California, USA
- Terneras mine, Velardeña, Durango, Mexico
- Carlingford, Co. Louth, Ireland
- Güneyce-_ Ikizdere area, Trabzon Province, Turkey
- Mt. Chapchachi, north of the Caspian Sea, Kazakhstan
- Nugrah, Saudi Arabia
Field-hunting tip
Where it forms: In limestone affected by high-grade contact metamorphism. If you start seeing wollastonite, garnet, calcite in float, you are in the right ground. Typical habit: fibrous, radial. Train your eye for that shape before scanning the outcrop.








