Kamiokite is a rare iron molybdenum oxide typically found in skarn deposits. It is best identified by its opaque, black metallic luster and its specific paragenesis with molybdenum-bearing minerals in metamorphosed ore bodies.
Is this kamiokite?
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 kamiokite with a known reference. Kamiokite sits at Mohs 3-4.5, 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 to submetallic.
- 4Match the color rangeCompare against the expected color range: iron black.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: hexagonal, tabular.
Often confused with
Kamiokite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside kamiokite
Minerals reported to co-occur with kamiokite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Fe₂Mo₃O₈
- Mohs hardness
- 3-4.5
- Density
- 5.96 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic to submetallic
- Transparency
- Opaque
- Crystal system
- Hexagonal
- Crystal habit
- Hexagonal, tabular
- Cleavage
- {0001}, perfect
- Rarity
- Rare
- Uses
- Collector, Scientific research
- Host rock
- In quartz-molybdenite stockwork veins associated with granite porphyry dikes (Japan); in fissure veins filled during low-grade regional metamorphism of basalt (Michigan, USA)
Where rockhounds find kamiokite
Classic worldwide localities
- Mohawk and Ahmeek mines, Keweenaw Co., Michigan, USA
- Kamioka Ag–Pb–Zn mine, Gifu Prefecture, Japan
- Carajas deposit, locality not otherwise specified, Brazil
Field-hunting tip
Where it forms: In quartz-molybdenite stockwork veins associated with granite porphyry dikes (Japan); in fissure veins filled during low-grade regional metamorphism of basalt (Michigan, USA). If you start seeing molybdenite, potassic feldspar, fluorite in float, you are in the right ground. Typical habit: hexagonal, tabular. Train your eye for that shape before scanning the outcrop.








