Heulandite-Na is a common member of the zeolite group often recognized by its distinct coffin-shaped crystal habit. Collectors prize it for its excellent association with other zeolites in basaltic vugs, typically forming clusters of tabular, pearly-lustered crystals.
Is this heulandite-na?
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-na with a known reference. Heulandite-Na sits at Mohs 3-4 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Heulandite-Na leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Heulandite-Na typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: white, colorless, yellow, pink, orange, brown.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals, coffin-shaped, crusts.
Often confused with
Heulandite-Na vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside heulandite-na
Minerals reported to co-occur with heulandite-na. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Na,Ca)₂₋₃Al₃(Al,Si)₂Si₁₃O₃₆·12H₂O
- Mohs hardness
- 3-4
- Density
- 2.1-2.2 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular Crystals, Coffin-shaped, Crusts
- Cleavage
- Perfect On {010}
- Rarity
- Common
- Uses
- Collector
- Host rock
- Basalt Cavities, Volcanic Amygdales
- Typical price
- $10-100 depending on specimen size and clarity
Where rockhounds find heulandite-na
Classic worldwide localities
- Nasik, India
- Teigarhorn, Iceland
- Fairfax Quarry, Virginia, USA
- Bay of Fundy, Nova Scotia, Canada
Field-hunting tip
Look in basalt cavities, volcanic amygdales country — that is the host setting where heulandite-na typically forms. If you start seeing quartz, apophyllite, calcite in float, you are in the right ground. Field specimens usually show a tabular crystals, coffin-shaped, crusts habit, so train your eye for that shape before scanning the outcrop.






