Gmelinite-Ca is a member of the zeolite group often found as sharp, rhombohedral crystals in volcanic amygdules. Collectors should look for its distinctive hexagonal habit, which can sometimes appear as complex interpenetrating twins, typically occurring in basaltic environments alongside other zeolites.
Is this gmelinite-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 gmelinite-ca with a known reference. Gmelinite-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. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: white, reddish white, pink, greenish white, flesh red.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: crystalline, druse.
Often confused with
Gmelinite-Ca vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside gmelinite-ca
Minerals reported to co-occur with gmelinite-ca. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₂(Si₈Al₄)O₂₄·11H₂O
- Mohs hardness
- 4.5
- Density
- 2.11 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Hexagonal
- Crystal habit
- Crystalline, druse
- Cleavage
- {10*0}, distinct; parting on {00*1}
- Rarity
- Uncommon
- Uses
- Collector
- Host rock
- Formed from calcium-rich fluids, in basalts and related igneous rocks, also pegmatites
Where rockhounds find gmelinite-ca
Classic worldwide localities
- Bergen Hill, Hudson Co., and Great Notch, Paterson, and Prospect Park, Passaic Co., New Jersey, USA
- Springfield, Lane Co., Oregon, USA
- Montecchio Maggiore, Vicenza, Italy
- Glenarm, in Co. Antrim, Ireland
- Isle of Skye, Scotland
- Pyrgos, Cyprus
Field-hunting tip
Where it forms: Formed from calcium-rich fluids, in basalts and related igneous rocks, also pegmatites. If you start seeing analcime, chabazite, calcite in float, you are in the right ground. Typical habit: crystalline, druse. Train your eye for that shape before scanning the outcrop.







