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, 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.





