Wairakite is a rare calcium-rich member of the zeolite group that is chemically and structurally similar to analcime. It is typically found as a secondary mineral in geothermal fields, occurring within altered volcanic rocks or deposited from hot springs. Collectors value it for its characteristic trapezohedral crystal habit, which often mimics the appearance of analcime.
Is this wairakite?
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 wairakite with a known reference. Wairakite sits at Mohs 5.5-6, 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 nearly dull.
- 4Match the color rangeCompare against the expected color range: white, colorless.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: trapezohedral crystals, granular, massive.
Often confused with
Wairakite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside wairakite
Minerals reported to co-occur with wairakite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaAl₂Si₄O₁₂·2H₂O
- Mohs hardness
- 5.5-6
- Density
- 2.26 g/cm³
- Streak
- White
- Luster
- Vitreous to nearly dull
- Transparency
- Transparent to translucent
- Crystal system
- Monoclinic
- Crystal habit
- Trapezohedral crystals, granular, massive
- Cleavage
- Two sets of possible partings intersecting at 90°
- Rarity
- Uncommon
- Uses
- Collector
- Host rock
- In pores and cavities in rocks in geothermal areas, deposited from hydrothermal fluids; may replace feldspar
Where rockhounds find wairakite
Classic worldwide localities
- Geysers, Sonoma Co., and near Rosamond, Kern Co., California, USA
- Yellowstone National Park, Wyoming, USA
- Mt. Rainier National Park, Pierce Co., Washington, USA
- North Island, at Wairakei, about six km north-northeast of Lake Taupo, and in the Tui mine, Te Aroha, Auckland, New Zealand
- St. Thomas and St. Croix, American Virgin Islands
- Buttle Lake area, Vancouver Island, British Columbia, Canada
Field-hunting tip
Where it forms: In pores and cavities in rocks in geothermal areas, deposited from hydrothermal fluids; may replace feldspar. If you start seeing andesine, epidote, clinozoisite in float, you are in the right ground. Typical habit: trapezohedral crystals, granular, massive. Train your eye for that shape before scanning the outcrop.









