Erionite-K is a member of the zeolite group that typically forms as delicate, hair-like fibers or woolly mats in volcanic environments. Collectors should be aware of its asbestiform nature, which requires strict safety protocols to prevent inhalation of hazardous fibers during specimen management.
Is this erionite-k?
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-k with a known reference. Erionite-K 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-K leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Erionite-K typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: white, colorless, pale yellow.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: acicular crystals, fibrous, woolly aggregates.
Often confused with
Erionite-K vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside erionite-k
Minerals reported to co-occur with erionite-k. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- K₂CaMg(Si₁₃Al₅)O₃₆·15H₂O
- Mohs hardness
- 3.5-4
- Density
- 2.1 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Hexagonal
- Crystal habit
- Acicular Crystals, Fibrous, Woolly Aggregates
- Cleavage
- None
- Rarity
- Uncommon
- Uses
- Collector, Scientific Research
- Host rock
- Volcanic Ash Beds, Basalt Cavities
- Typical price
- $20-100 per specimen
Where rockhounds find erionite-k
Classic worldwide localities
- Durkee, Oregon, USA
- Jersey Valley, Nevada, USA
- Rome, Oregon, USA
- Antrim, Northern Ireland
Field-hunting tip
Look in volcanic ash beds, basalt cavities country — that is the host setting where erionite-k typically forms. If you start seeing chabazite, phillipsite, calcite in float, you are in the right ground. Field specimens usually show a acicular crystals, fibrous, woolly aggregates habit, so train your eye for that shape before scanning the outcrop.






