Akaogiite is a rare monoclinic polymorph of titanium dioxide that forms as a high-pressure alteration product. It is primarily found as microscopic inclusions or thin platy crystals within granite pegmatites and is scientifically significant for its unique structural arrangement compared to more common TiO₂ polymorphs.
Is this akaogiite?
3-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 akaogiite with a known reference. Akaogiite sits at Mohs 6, softer than the next harder reference, harder than the previous one.
- 2Match the color rangeCompare against the expected color range: black, brown.
- 3Look at form & habitCrystal system: monoclinic. Typical habit: platy crystals.
Often confused with
Akaogiite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside akaogiite
Minerals reported to co-occur with akaogiite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- TiO₂
- Mohs hardness
- 6
- Density
- 4.72 g/cm³
- Transparency
- Opaque
- Crystal system
- Monoclinic
- Crystal habit
- Platy crystals
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Within multiphase TiO2 clusters enclosed in biotite in heavily shocked garnet-cordierite-sillimanite gneiss in the breccia of a meteorite impact crater
Where rockhounds find akaogiite
Classic worldwide localities
- Ries meteorite impact crater, Germany
Field-hunting tip
Where it forms: Within multiphase TiO2 clusters enclosed in biotite in heavily shocked garnet-cordierite-sillimanite gneiss in the breccia of a meteorite impact crater. If you start seeing rutile, ilmenite, titanite in float, you are in the right ground. Typical habit: platy crystals. Train your eye for that shape before scanning the outcrop.






