Changchengite is an extremely rare iridium bismuth telluride mineral first discovered in the Changcheng gold mine in China. It typically occurs as minute, metallic grey grains embedded within massive sulfide ore, requiring advanced mineralogical analysis for identification.
Is this changchengite?
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 changchengite with a known reference. Changchengite sits at Mohs 3.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Changchengite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Changchengite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: gray, white.
- 5Look at form & habitCrystal system: cubic. Typical habit: anhedral grains.
Often confused with
Changchengite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside changchengite
Minerals reported to co-occur with changchengite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- IrBiTe
- Mohs hardness
- 3.5
- Density
- 9.2 g/cm³
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Cubic
- Crystal habit
- Anhedral Grains
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Veins
- Typical price
- $500+ per specimen
Where rockhounds find changchengite
Classic worldwide localities
- Changcheng mine, Hebei Province, China
Field-hunting tip
Look in hydrothermal veins country — that is the host setting where changchengite typically forms. If you start seeing chalcopyrite, pyrite, galena 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.






