Cuproauride is a rare intermetallic mineral composed of copper and gold. It typically occurs as microscopic grains within gold-bearing veins or volcanic environments and is highly prized by collectors for its unique chemical composition.
Is this cuproauride?
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 cuproauride with a known reference. Cuproauride sits at Mohs 2.5-3 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Cuproauride leaves a yellow streak.
- 3Read the lusterHold the specimen under a strong light. Cuproauride typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: yellow, gold-yellow.
- 5Look at form & habitCrystal system: cubic. Typical habit: anhedral grains, massive, interstitial fillings.
Often confused with
Cuproauride vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside cuproauride
Minerals reported to co-occur with cuproauride. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CuAu
- Mohs hardness
- 2.5-3
- Density
- 15.0-16.0 g/cm³
- Colors
- Streak
- Yellow
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Cubic
- Crystal habit
- Anhedral Grains, Massive, Interstitial Fillings
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector, Scientific Research
- Host rock
- Hydrothermal Veins, Volcanic Exhalations
- Typical price
- $50-500 depending on specimen size and rarity
Where rockhounds find cuproauride
Classic worldwide localities
- Hope's Nose, Torquay, UK
- Kudryavyi Volcano, Kuril Islands, Russia
- Komsomolskoye gold deposit, Kazakhstan
Field-hunting tip
Look in hydrothermal veins, volcanic exhalations country — that is the host setting where cuproauride typically forms. If you start seeing gold, hematite, cuprite in float, you are in the right ground. Field specimens usually show a anhedral grains, massive, interstitial fillings habit, so train your eye for that shape before scanning the outcrop.





