Breyite is a rare high-pressure polymorph of calcium silicate found as inclusions within diamonds originating from the Earth's lower mantle. Because it only forms under extreme deep-earth conditions, it is almost exclusively identified through microscopic analysis of diamond-hosted grains.
Is this breyite?
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 breyite with a known reference. Breyite sits at Mohs 7-7.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Breyite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Breyite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, white.
- 5Look at form & habitCrystal system: tetragonal. Typical habit: microscopic inclusions.
Often confused with
Breyite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside breyite
Minerals reported to co-occur with breyite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaSiO₃
- Mohs hardness
- 7-7.5
- Density
- 3.37 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Tetragonal
- Crystal habit
- Microscopic Inclusions
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector, Scientific Research
- Host rock
- Lower Mantle Xenoliths
- Typical price
- n/a (research specimens only)
Where rockhounds find breyite
Classic worldwide localities
- Brazil
- South Africa
- Russia
Field-hunting tip
Look in lower mantle xenoliths country, the host setting where breyite typically forms. If you start seeing diamond, olivine, enstatite in float, you are in the right ground. Field specimens usually show a microscopic inclusions habit, so train your eye for that shape before scanning the outcrop.




