Vaterite is a rare polymorph of calcium carbonate that is metastable under ambient conditions, often transforming into calcite or aragonite over time. It is frequently identified in nature as microscopic spherulitic aggregates within sedimentary environments or associated with biogenic minerals in organisms.
Is this vaterite?
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 vaterite with a known reference. Vaterite sits at Mohs 3 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Vaterite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Vaterite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: white, colorless.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: spherulitic.
Often confused with
Vaterite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside vaterite
Minerals reported to co-occur with vaterite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaCO₃
- Mohs hardness
- 3
- Density
- 2.65 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Hexagonal
- Crystal habit
- Spherulitic
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector, Scientific Research
- Host rock
- Low-temperature Hydrothermal Environments and Biological Precipitates
- Typical price
- $20-100 per specimen
Where rockhounds find vaterite
Classic worldwide localities
- Larne, Northern Ireland
- Shimane Prefecture, Japan
- Cumberland, England
- Czech Republic
Field-hunting tip
Look in low-temperature hydrothermal environments and biological precipitates country — that is the host setting where vaterite typically forms. If you start seeing calcite, aragonite, portlandite in float, you are in the right ground. Field specimens usually show a spherulitic habit, so train your eye for that shape before scanning the outcrop.



