Garronite-Ca is a member of the zeolite group found primarily in the vesicles of basaltic rocks. Collectors look for its distinctive white or colorless radiating aggregates which are often found alongside other zeolites like chabazite or phillipsite.
Is this garronite-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 garronite-ca with a known reference. Garronite-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. Garronite-Ca leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Garronite-Ca typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: white, colorless, yellowish, pinkish.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: pseudotetragonal crystals, radiating aggregates, massive.
Often confused with
Garronite-Ca vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside garronite-ca
Minerals reported to co-occur with garronite-ca. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- NaCa₂₅Al₅₂Si₁₃₂O₃₆₈·nH₂O
- Mohs hardness
- 4.5
- Density
- 2.12-2.14 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Pseudotetragonal Crystals, Radiating Aggregates, Massive
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Amygdaloidal Basalt Cavities
- Typical price
- $20-150 depending on specimen size and quality
Where rockhounds find garronite-ca
Classic worldwide localities
- Garron Plateau, Northern Ireland
- Skye, Scotland
- Iceland
- Faeroe Islands
- Melbourne, Victoria, Australia
Field-hunting tip
Look in amygdaloidal basalt cavities country — that is the host setting where garronite-ca typically forms. If you start seeing chabazite, thomsonite, phillipsite in float, you are in the right ground. Field specimens usually show a pseudotetragonal crystals, radiating aggregates, massive habit, so train your eye for that shape before scanning the outcrop.





