Bridgmanite is the most abundant mineral in Earth, making up the majority of the lower mantle, but it is extremely rare at the surface. It is primarily found as microscopic inclusions within shock-metamorphosed meteorites that originated from the deep mantle of terrestrial bodies. It is a high-pressure polymorph of silicate perovskite that requires extreme conditions to exist.
Is this bridgmanite?
2-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 bridgmanite with a known reference. Bridgmanite sits at Mohs 6-6.5, softer than the next harder reference, harder than the previous one.
- 2Look at form & habitCrystal system: orthorhombic. Typical habit: massive, anhedral grains.
Often confused with
Bridgmanite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside bridgmanite
Minerals reported to co-occur with bridgmanite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- MgSiO₃
- Mohs hardness
- 6-6.5
- Density
- 4.1 g/cm³
- Transparency
- Opaque
- Crystal system
- Orthorhombic
- Crystal habit
- Massive, anhedral grains
- Rarity
- Rare
- Uses
- Scientific study, Collector
- Host rock
- The dominant mineral of the silicate lower mantle of the Earth
Where rockhounds find bridgmanite
Classic worldwide localities
- Tenham meteorite
- Suizhou meteorite
Field-hunting tip
Where it forms: The dominant mineral of the silicate lower mantle of the Earth. If you start seeing akimotoite, ringwoodite, majorite in float, you are in the right ground. Typical habit: massive, anhedral grains. Train your eye for that shape before scanning the outcrop.






