Stannoidite is a rare copper-iron-tin sulfide mineral typically found in hydrothermal vein deposits. It is often identified by its distinct bronze color and metallic luster, usually occurring as massive grains rather than well-formed crystals.
Is this stannoidite?
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 stannoidite with a known reference. Stannoidite sits at Mohs ~4, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: dark brown-gray.
- 3Read the lusterHold the specimen under a strong light. Luster: metallic.
- 4Match the color rangeCompare against the expected color range: brass brown.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: massive.
Often confused with
Stannoidite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside stannoidite
Minerals reported to co-occur with stannoidite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Cu₈Fe₂(Fe,Zn)Sn₂S₁₂
- Mohs hardness
- ~4
- Density
- 4.29 g/cm³
- Colors
- Brass brown
- Streak
- Dark brown-gray
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Orthorhombic
- Crystal habit
- Massive
- Cleavage
- None
- Rarity
- Uncommon
- Uses
- Collector
- Host rock
- In hydrothermal Sn–Cu sulfide deposits
Where rockhounds find stannoidite
Classic worldwide localities
- Campbell mine, Bisbee, Cochise Co., Arizona, and at Butte, Silver Bow Co., Montana, USA
- Konjo mine, Okayama Prefecture (type locality), Japan
- Fukoku mine, Kyoto Prefecture, Japan
- Hyogo Prefecture, at the Ikuno mine, Kanagase, Japan
- Akenobe mine, Yabu, Japan
- Tingha, New South Wales, Australia
Field-hunting tip
Where it forms: In hydrothermal Sn–Cu sulfide deposits. If you start seeing chalcopyrite, galena, tetrahedrite in float, you are in the right ground. Typical habit: massive. Train your eye for that shape before scanning the outcrop.








