Ishikawaite is a rare, radioactive niobium-tantalum mineral found primarily in granitic pegmatites. It usually presents as black to brownish-black prismatic crystals or irregular masses, often requiring a Geiger counter for positive identification in the field.
Is this ishikawaite?
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 ishikawaite with a known reference. Ishikawaite sits at Mohs 5-6, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: dark brown to black.
- 3Read the lusterHold the specimen under a strong light. Luster: waxy, resinous to vitreous.
- 4Match the color rangeCompare against the expected color range: black.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: metamict.
Often confused with
Ishikawaite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside ishikawaite
Minerals reported to co-occur with ishikawaite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (U,Fe,Y)NbO₄
- Mohs hardness
- 5-6
- Density
- 6.2-6.4 g/cm³
- Colors
- Streak
- Dark brown to black
- Luster
- Waxy, resinous to vitreous
- Transparency
- Opaque
- Crystal system
- Orthorhombic
- Crystal habit
- Metamict
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector, Research
- Host rock
- In pegmatite, and alluvium (Ishikawa district, Japan); as micro-inclusions in vitrophyre clasts in highly differentiated, rare-element rich, pyroclastic rhyolites (Honeycomb Hills, USA)
Where rockhounds find ishikawaite
Classic worldwide localities
- Ishikawa district, Fukushima Prefecture, Japan
- Reported from other localities in Japan, but confirmation is impossible
- Kunar, Afghanistan
- Honeycomb Hills, Juab Co., Utah, USA, for example, seems very similar but is regarded as uranoan samarskite
Field-hunting tip
Where it forms: In pegmatite, and alluvium (Ishikawa district, Japan); as micro-inclusions in vitrophyre clasts in highly differentiated, rare-element rich, pyroclastic rhyolites (Honeycomb Hills, USA). If you start seeing samarskite, ferrocolumbite in float, you are in the right ground. Typical habit: metamict. Train your eye for that shape before scanning the outcrop.


