Sugakiite is a rare copper-iron sulfide mineral typically found in intimate intergrowths within skarn-type ore deposits. It is primarily identified in polished sections via microscopic examination due to its extremely small grain size and similarity to other copper-iron sulfides.
Is this sugakiite?
4-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 sugakiite with a known reference. Sugakiite sits at Mohs 2-3, softer than the next harder reference, harder than the previous one.
- 2Read the lusterHold the specimen under a strong light. Luster: metallic.
- 3Match the color rangeCompare against the expected color range: reddish yellow.
- 4Look at form & habitCrystal system: tetragonal. Typical habit: granular.
Often confused with
Sugakiite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside sugakiite
Minerals reported to co-occur with sugakiite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Cu(Fe,Ni)₈S₈
- Mohs hardness
- 2-3
- Density
- 4.71 g/cm³
- Colors
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Tetragonal
- Crystal habit
- Granular
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- An intergranular exsolved phase in sulfide aggregates in lherzolite in a peridotite massif
Where rockhounds find sugakiite
Classic worldwide localities
- Horoman peridotite massif, Samanicho, Samani-gun, Hokkaido, Japan
Field-hunting tip
Where it forms: An intergranular exsolved phase in sulfide aggregates in lherzolite in a peridotite massif. If you start seeing bornite, talnakhite, copper in float, you are in the right ground. Typical habit: granular. Train your eye for that shape before scanning the outcrop.






