Kitagohaite is a very rare platinum-copper alloy typically found as microscopic grains within ultramafic rock complexes. It is primarily identified through electron microprobe analysis rather than visual field inspection due to its extremely small, metallic white appearance.
Is this kitagohaite?
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 kitagohaite with a known reference. Kitagohaite sits at Mohs 3.5-4 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Kitagohaite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Kitagohaite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: white, silver-white.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: anhedral grains.
Often confused with
Kitagohaite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside kitagohaite
Minerals reported to co-occur with kitagohaite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pt₃Cu
- Mohs hardness
- 3.5-4
- Density
- 16.4 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Hexagonal
- Crystal habit
- Anhedral Grains
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Ultramafic Rocks
- Typical price
- $50-500+ per microscopic specimen
Where rockhounds find kitagohaite
Classic worldwide localities
- Kitagoha, Japan
Field-hunting tip
Look in ultramafic rocks country — that is the host setting where kitagohaite typically forms. If you start seeing platinum, cooperite, chromite in float, you are in the right ground. Field specimens usually show a anhedral grains habit, so train your eye for that shape before scanning the outcrop.




