Ringwoodite is a high-pressure polymorph of olivine that exists deep within the Earth's mantle transition zone between 520 and 660 kilometers deep. Because it is rarely brought to the surface except via meteorites or as rare inclusions in deep-seated diamonds, it is an exceptionally rare find for collectors and scientists alike.
Is this ringwoodite?
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 ringwoodite with a known reference. Ringwoodite sits at Mohs 6.5-7 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Ringwoodite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Ringwoodite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: blue, purple, colorless.
- 5Look at form & habitCrystal system: cubic. Typical habit: microscopic granular aggregates.
Often confused with
Ringwoodite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside ringwoodite
Minerals reported to co-occur with ringwoodite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Mg,Fe)₂SiO₄
- Mohs hardness
- 6.5-7
- Density
- 3.84 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Cubic
- Crystal habit
- Microscopic Granular Aggregates
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector, Scientific Research
- Host rock
- Deep-mantle Transition Zone
- Typical price
- $500-5000+ per microscopic specimen
Where rockhounds find ringwoodite
Classic worldwide localities
- Tenham meteorite (Australia)
- Grandidierite inclusions
- Deep Earth mantle samples
Field-hunting tip
Look in deep-mantle transition zone country — that is the host setting where ringwoodite typically forms. If you start seeing bridgmanite, wadsleyite, majorite in float, you are in the right ground. Field specimens usually show a microscopic granular aggregates habit, so train your eye for that shape before scanning the outcrop.




