Takanawaite-(Y) is an extremely rare yttrium tantalum oxide mineral that was first identified in the Takanawa Peninsula of Japan. It typically appears as small granular or massive aggregates within granitic pegmatite environments, often associated with other rare earth minerals. Due to its scarcity and radioactivity, it is primarily sought after by advanced systematic mineral collectors.
Is this takanawaite-(y)?
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 takanawaite-(y) with a known reference. Takanawaite-(Y) sits at Mohs 5.5, softer than the next harder reference, harder than the previous one.
- 2Match the color rangeCompare against the expected color range: dark brown.
- 3Look at form & habitCrystal system: monoclinic. Typical habit: granular to massive.
Often found alongside takanawaite-(y)
Minerals reported to co-occur with takanawaite-(y). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- YTaO₄
- Mohs hardness
- 5.5
- Density
- 6.97 g/cm³
- Colors
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Granular to massive
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In pegmatites in granite
Where rockhounds find takanawaite-(y)
Classic worldwide localities
- Takanawa Mountain, near Matsuyama City, Ehime Prefecture, Japan
Field-hunting tip
Where it forms: In pegmatites in granite. If you start seeing gadolinite-, zircon, muscovite in float, you are in the right ground. Typical habit: granular to massive. Train your eye for that shape before scanning the outcrop.




