Cave pearls are small, rounded, spherical or ovoid concretions of calcite that form in limestone caves through the deposition of calcium carbonate around a nucleus. They are typically found in shallow cave pools where dripping water keeps the pearls in constant motion, preventing them from cementing to the pool floor.
Is this cave pearls?
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 cave pearls with a known reference. Cave Pearls 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. Cave Pearls leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Cave Pearls typically shows a dull luster.
- 4Match the color rangeCompare against the expected color range: white, cream, gray, brown.
- 5Look at form & habitCrystal system: trigonal. Typical habit: spherical or ovoid concretionary aggregates.
Often found alongside cave pearls
Minerals reported to co-occur with cave pearls. 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
- 2.71 g/cm³
- Streak
- White
- Luster
- Dull
- Transparency
- Opaque
- Crystal system
- Trigonal
- Crystal habit
- Spherical or Ovoid Concretionary Aggregates
- Cleavage
- Perfect Rhombohedral
- Fluorescence
- Often Exhibits White or Yellow Under UV
- Rarity
- Common
- Uses
- Collector, Educational
- Host rock
- Limestone Solution Caves
- Typical price
- $10-100 per specimen depending on size and luster
Where rockhounds find cave pearls
Classic worldwide localities
- Carlsbad Caverns, USA
- Lechuguilla Cave, USA
- Postojna Cave, Slovenia
- Grutas de Cacahuamilpa, Mexico
Field-hunting tip
Look in limestone solution caves country — that is the host setting where cave pearls typically forms. If you start seeing calcite, aragonite in float, you are in the right ground. Field specimens usually show a spherical or ovoid concretionary aggregates habit, so train your eye for that shape before scanning the outcrop.


