Heulandite-Ca is a common member of the zeolite group, best recognized by its characteristic 'coffin-shaped' tabular crystals. It is frequently found in the cavities of basaltic rocks, often occurring in dense, attractive clusters associated with other zeolites and minerals like stilbite or apophyllite.
Is this heulandite-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 heulandite-ca with a known reference. Heulandite-Ca sits at Mohs 3-3.5, 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 to pearly.
- 4Match the color rangeCompare against the expected color range: white, reddish white, grayish white, brownish white, yellow.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: crystalline, tabular.
Often confused with
Heulandite-Ca vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside heulandite-ca
Minerals reported to co-occur with heulandite-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)₅(Si₂₇Al₉)O₇₂·26H₂O
- Mohs hardness
- 3-3.5
- Density
- 2.2 g/cm³
- Streak
- White
- Luster
- Vitreous to pearly
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Crystalline, tabular
- Cleavage
- Perfect on {010}
- Rarity
- Common
- Uses
- Collector, Specimen
- Host rock
- Low temperature zeolite found in a wide variety of geologic environments: volcanic rocks, metamorphic rocks, pegmatites, tuffs, and deep-sea sediments
Where rockhounds find heulandite-ca
Classic worldwide localities
- Glasgow, Strathclyde (Dumbartonshire), Scotland (type locality)
Field-hunting tip
Where it forms: Low temperature zeolite found in a wide variety of geologic environments: volcanic rocks, metamorphic rocks, pegmatites, tuffs, and deep-sea sediments. If you start seeing stilbite, apophyllite, calcite in float, you are in the right ground. Typical habit: crystalline, tabular. Train your eye for that shape before scanning the outcrop.






