Wadalite is a rare calcium-aluminum silicate chloride mineral typically occurring as small, transparent dodecahedral crystals. It is primarily found in contact-metamorphosed limestone xenoliths within volcanic rocks, often requiring microscopic study for positive identification.
Is this wadalite?
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 wadalite with a known reference. Wadalite sits at Mohs 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.
- 4Match the color rangeCompare against the expected color range: colorless.
- 5Look at form & habitCrystal system: cubic. Typical habit: dodecahedral crystals.
Often confused with
Wadalite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside wadalite
Minerals reported to co-occur with wadalite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₆Al₅Si₂O₁₆Cl₃
- Mohs hardness
- 6
- Density
- 3.06 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Cubic
- Crystal habit
- Dodecahedral crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Skarn xenolith in two-pyroxene andesite
Where rockhounds find wadalite
Classic worldwide localities
- Tadano, Koriyama Cith, Fukushima Prefecture, Japan (type locality)
Field-hunting tip
Where it forms: Skarn xenolith in two-pyroxene andesite. If you start seeing gehlenite, spinell, perovskite in float, you are in the right ground. Typical habit: dodecahedral crystals. Train your eye for that shape before scanning the outcrop.



