Cupalite is an extremely rare copper-aluminum intermetallic mineral found primarily in placer deposits. It typically occurs as small, metallic grains with a distinct copper-steel-yellow color and is often only identifiable through specialized microscopic and chemical analysis.
Is this cupalite?
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 cupalite with a known reference. Cupalite sits at Mohs 4.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: copper-red.
- 3Read the lusterHold the specimen under a strong light. Luster: metallic.
- 4Match the color rangeCompare against the expected color range: steel yellow.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: inclusions, microscopic crystals.
Often confused with
Cupalite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside cupalite
Minerals reported to co-occur with cupalite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CuAl
- Mohs hardness
- 4.5
- Density
- 5.12 g/cm³
- Colors
- Steel yellow
- Streak
- Copper-red
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Orthorhombic
- Crystal habit
- Inclusions, microscopic crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In black slick washed from greenish gray cover weathering from serpentine
Where rockhounds find cupalite
Classic worldwide localities
- Listvenitovii stream, Khatirskii ultramafic zone of the Koryak-Kamchata fold area, Koryak Mountains, USSR
Field-hunting tip
Where it forms: In black slick washed from greenish gray cover weathering from serpentine. If you start seeing khatyrkite in float, you are in the right ground. Typical habit: inclusions, microscopic crystals. Train your eye for that shape before scanning the outcrop.


