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, 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.




