Lisetite is a rare high-pressure polymorph of calcium aluminum silicate found within eclogites. It typically occurs as small grains in high-grade metamorphic environments, making it a significant mineral for understanding crustal subduction processes.
Is this lisetite?
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 lisetite with a known reference. Lisetite 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. Lisetite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Lisetite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: white, colorless, gray.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: anhedral to subhedral grains.
Often confused with
Lisetite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside lisetite
Minerals reported to co-occur with lisetite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaAl₂Si₂O₈
- Mohs hardness
- 6
- Density
- 2.68 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Anhedral to Subhedral Grains
- Cleavage
- Perfect On {001} and {010}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Eclogite Facies Rocks
- Typical price
- $20-100 per specimen
Where rockhounds find lisetite
Classic worldwide localities
- Liset, Norway
Field-hunting tip
Look in eclogite facies rocks country, the host setting where lisetite typically forms. If you start seeing garnet, pyroxene, kyanite in float, you are in the right ground. Field specimens usually show a anhedral to subhedral grains habit, so train your eye for that shape before scanning the outcrop.





