Phillipsite is a common zeolite mineral recognized by its distinctive, complex cross-shaped penetration twins. It typically forms within the cavities of volcanic rocks like basalt, often appearing as white or colorless radiating clusters.
Is this phillipsite?
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 phillipsite with a known reference. Phillipsite sits at Mohs 4-5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Phillipsite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Phillipsite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: white, colorless, yellow, red, brown.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: complex cruciform penetration twins, radiating aggregates.
Often confused with
Phillipsite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside phillipsite
Minerals reported to co-occur with phillipsite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (K,Na,Ca)₁₋₃(Si,Al)₈O₁₆·6H₂O
- Mohs hardness
- 4-5
- Density
- 2.2 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Complex Cruciform Penetration Twins, Radiating Aggregates
- Cleavage
- Distinct On {010}
- Rarity
- Common
- Uses
- Collector, Scientific Research
- Host rock
- Basaltic Vugs and Cavities
- Typical price
- $5-30 per specimen
Where rockhounds find phillipsite
Classic worldwide localities
- Sicily, Italy
- Giant's Causeway, Northern Ireland
- Iceland
- Table Mountain, Colorado, USA
- Victoria, Australia
Field-hunting tip
Look in basaltic vugs and cavities country — that is the host setting where phillipsite typically forms. If you start seeing chabazite, natrolite, calcite in float, you are in the right ground. Field specimens usually show a complex cruciform penetration twins, radiating aggregates habit, so train your eye for that shape before scanning the outcrop.






