Changchengite is an extremely rare iridium bismuth telluride mineral first discovered in the Changcheng gold mine in China. It typically occurs as minute, steel-black 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 3.7, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: black.
- 3Read the lusterHold the specimen under a strong light. Luster: metallic.
- 4Match the color rangeCompare against the expected color range: gray, black.
- 5Look at form & habitCrystal system: cubic. Typical habit: granular.
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
- Ir(BiS)
- Mohs hardness
- 3.7
- Density
- 11.96-12.27 g/cm³
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Cubic
- Crystal habit
- Granular
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Of hydrothermal origin in chromite bodies in dunites and placers derived therefrom
Where rockhounds find changchengite
Classic worldwide localities
- Along a branch of the Luanhe River in Hebei Province, about 200 km ENE of Beijing, China (type locality)
Field-hunting tip
Where it forms: Of hydrothermal origin in chromite bodies in dunites and placers derived therefrom. If you start seeing iridium, ferrian platinum, laurite in float, you are in the right ground. Typical habit: granular. Train your eye for that shape before scanning the outcrop.






