Paulingite-Ca is a complex and highly sought-after zeolite species characterized by its intricate cubic crystal structures. Collectors typically find these as tiny, sharp rhombic dodecahedrons lining cavities in basaltic rocks, often requiring magnification for full appreciation of their geometric perfection.
Is this paulingite-ca?
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 paulingite-ca with a known reference. Paulingite-Ca sits at Mohs 4-5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Paulingite-Ca leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Paulingite-Ca typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, white.
- 5Look at form & habitCrystal system: cubic. Typical habit: rhombic dodecahedral crystals.
Often confused with
Paulingite-Ca vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside paulingite-ca
Minerals reported to co-occur with paulingite-ca. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Ca,Na,K)₁₀₀(Si,Al)₃₈₄O₇₆₈·nH₂O
- Mohs hardness
- 4-5
- Density
- 2.1-2.2 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Cubic
- Crystal habit
- Rhombic Dodecahedral Crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Vesicles in Basaltic or Alkaline Igneous Rocks
- Typical price
- $50-500 depending on specimen size and clarity
Where rockhounds find paulingite-ca
Classic worldwide localities
- Varennes, Quebec, Canada
- Rjukan, Norway
- Columbia River Basalt Group, USA
- Teigarhorn, Iceland
Field-hunting tip
Look in vesicles in basaltic or alkaline igneous rocks country — that is the host setting where paulingite-ca typically forms. If you start seeing calcite, thomsonite, heulandite in float, you are in the right ground. Field specimens usually show a rhombic dodecahedral crystals habit, so train your eye for that shape before scanning the outcrop.






