Erionite-Ca is a rare fibrous zeolite that typically forms delicate, needle-like crystals in volcanic rocks. It is most famous for its link to serious respiratory health issues in regions where erionite-rich dust is present, making it a mineral of extreme interest for both its geological occurrence and its biological hazards.
Is this erionite-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 erionite-ca with a known reference. Erionite-Ca 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. Erionite-Ca leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Erionite-Ca typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: white, colorless, yellowish.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: acicular or fibrous radial aggregates.
Often confused with
Erionite-Ca vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside erionite-ca
Minerals reported to co-occur with erionite-ca. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₂KNa(Si₂₇Al₉)O₇₂·28H₂O
- Mohs hardness
- 3.5-4
- Density
- 2.09 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Hexagonal
- Crystal habit
- Acicular or Fibrous Radial Aggregates
- Cleavage
- Good On {10-10}
- Rarity
- Rare
- Uses
- Collector, Scientific Research
- Host rock
- Volcanic Cavities and Ash Flow Tuffs
- Typical price
- $20-100 per specimen
Where rockhounds find erionite-ca
Classic worldwide localities
- Oregon, USA
- Nevada, USA
- Iceland
- Italy
- New Zealand
Field-hunting tip
Look in volcanic cavities and ash flow tuffs country — that is the host setting where erionite-ca typically forms. If you start seeing calcite, phillipsite, chabazite in float, you are in the right ground. Field specimens usually show a acicular or fibrous radial aggregates habit, so train your eye for that shape before scanning the outcrop.






