Kuratite is an exceptionally rare mineral primarily identified within carbonaceous chondrite meteorites. It typically occurs as small grains associated with other silicate and metallic phases in extraterrestrial material.
Is this kuratite?
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 kuratite with a known reference. Kuratite sits at Mohs 6-7, softer than the next harder reference, harder than the previous one.
- 2Look at form & habitCrystal system: triclinic. Typical habit: granular aggregates, interstitial grains.
Often confused with
Kuratite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside kuratite
Minerals reported to co-occur with kuratite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₂(Fe₅Ti)O₂[Si₄Al₂O₁₈]
- Mohs hardness
- 6-7
- Density
- 3.906 g/cm³
- Transparency
- Opaque
- Crystal system
- Triclinic
- Crystal habit
- Granular aggregates, interstitial grains
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In multiple-phase pockets, located mainly at olivine-augite triple junctions in an angrite meteorite, probably crystallized from an interstitial melt
Where rockhounds find kuratite
Classic worldwide localities
- Puy de Saint-Sandoux, Auvergne, France
- Foster Crater, McMurdo Volcanic Group, Antarctica and Saint-Leu, Réunion Island
- Kaiserstuhl volcanic complex, Upper Rhine Graben, SW Germany
Field-hunting tip
Where it forms: In multiple-phase pockets, located mainly at olivine-augite triple junctions in an angrite meteorite, probably crystallized from an interstitial melt. If you start seeing whitlockite, ulvöspinel, ca-rich fayalite in float, you are in the right ground. Typical habit: granular aggregates, interstitial grains. Train your eye for that shape before scanning the outcrop.



