Gobbinsite is a rare zeolite mineral that typically forms small, white pseudocubic crystals within cavities of basaltic rocks. It is best identified through its characteristic interpenetrant twinning and association with other zeolites like phillipsite.
Is this gobbinsite?
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 gobbinsite with a known reference. Gobbinsite sits at Mohs ~4, 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: lemon white, chalky white, light brown.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: aggregates, lath.
Often confused with
Gobbinsite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside gobbinsite
Minerals reported to co-occur with gobbinsite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₅(Si₁₁Al₅)O₃₂·11H₂O
- Mohs hardness
- ~4
- Density
- 2.194 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent to translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Aggregates, lath
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A secondary mineral in amygdules in basalts (Co. Antrim, Ireland); in cavities in sodalite syenite in an intrusive alkalic gabbro-syenite complex (Mont Saint-Hilaire, Canada)
Where rockhounds find gobbinsite
Classic worldwide localities
- Island Magee, from Two Mouth Cave, at the coastal escarpment near Hills Port, south of The Gobbins, and at Dunseverick, near Giant's Causeway, Co. Antrim, Ireland
- Mont Saint-Hilaire, Quebec, Canada
Field-hunting tip
Where it forms: A secondary mineral in amygdules in basalts (Co. Antrim, Ireland); in cavities in sodalite syenite in an intrusive alkalic gabbro-syenite complex (Mont Saint-Hilaire, Canada). If you start seeing gmelinite, calcite, tetranatrolite in float, you are in the right ground. Typical habit: aggregates, lath. Train your eye for that shape before scanning the outcrop.




