Stilbite-Na is most recognizable for its distinctive bowtie-shaped or sheaf-like crystal aggregates. It is a common zeolite found primarily in the cavities of basaltic volcanic rocks, often occurring in beautiful, aesthetic clusters alongside other zeolites like heulandite and apophyllite.
Is this stilbite-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 stilbite-na with a known reference. Stilbite-Na sits at Mohs 3.5-4 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Stilbite-Na leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Stilbite-Na typically shows a vitreous to pearly luster.
- 4Match the color rangeCompare against the expected color range: white, yellow, pink, orange, brown, colorless.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: sheaf-like aggregates, tabular crystals, bladed.
Often confused with
Stilbite-Na vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside stilbite-na
Minerals reported to co-occur with stilbite-na. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na(Si₂₇Al₉)O₇₂·28H₂O
- Mohs hardness
- 3.5-4
- Density
- 2.1-2.2 g/cm³
- Streak
- White
- Luster
- Vitreous to Pearly
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Sheaf-like Aggregates, Tabular Crystals, Bladed
- Cleavage
- Perfect On {010}
- Rarity
- Common
- Uses
- Collector, Specimen
- Host rock
- Basalt Cavities, Volcanic Amygdules
- Typical price
- $10-150 depending on specimen size and quality
Where rockhounds find stilbite-na
Classic worldwide localities
- Nashik, India
- Teigarhorn, Iceland
- Poona, India
- Nova Scotia, Canada
- New Jersey, USA
Field-hunting tip
Look in basalt cavities, volcanic amygdules country — that is the host setting where stilbite-na typically forms. If you start seeing heulandite, apophyllite, quartz in float, you are in the right ground. Field specimens usually show a sheaf-like aggregates, tabular crystals, bladed habit, so train your eye for that shape before scanning the outcrop.







