Pseudowollastonite is a high-temperature polymorph of CaSiO₃ that forms under specific contact metamorphic conditions. It is typically found in altered limestone xenoliths within volcanic rocks, often appearing as glassy, tabular crystals that are difficult to distinguish from common wollastonite without laboratory analysis.
Is this pseudowollastonite?
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 pseudowollastonite with a known reference. Pseudowollastonite sits at Mohs 4.5-5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Pseudowollastonite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Pseudowollastonite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: white, colorless, gray.
- 5Look at form & habitCrystal system: triclinic. Typical habit: tabular crystals, massive.
Often confused with
Pseudowollastonite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside pseudowollastonite
Minerals reported to co-occur with pseudowollastonite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaSiO₃
- Mohs hardness
- 4.5-5
- Density
- 2.90 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Triclinic
- Crystal habit
- Tabular Crystals, Massive
- Cleavage
- Good
- Rarity
- Rare
- Uses
- Collector, Scientific Research
- Host rock
- Metamorphosed Limestone
- Typical price
- $20-100 per specimen
Where rockhounds find pseudowollastonite
Classic worldwide localities
- Scawt Hill, Northern Ireland
- Kilchoan, Scotland
- Velardena, Mexico
- Bellerberg, Germany
Field-hunting tip
Look in metamorphosed limestone country — that is the host setting where pseudowollastonite typically forms. If you start seeing larnite, merwinite, gehlenite in float, you are in the right ground. Field specimens usually show a tabular crystals, massive habit, so train your eye for that shape before scanning the outcrop.






