Athabascaite is a rare copper selenide mineral typically found as massive, silver-white grains within hydrothermal ore deposits. It is best identified through laboratory analysis of its metallic luster and distinct chemical composition, as it often appears visually similar to other copper selenide species.
Is this athabascaite?
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 athabascaite with a known reference. Athabascaite sits at Mohs 3 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Athabascaite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Athabascaite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: silver-white, gray.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: massive, anhedral grains.
Often confused with
Athabascaite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside athabascaite
Minerals reported to co-occur with athabascaite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Cu₅Se₄
- Mohs hardness
- 3
- Density
- 8.55 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Orthorhombic
- Crystal habit
- Massive, Anhedral Grains
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Vein Deposits
- Typical price
- $50-300 per specimen depending on size and provenance
Where rockhounds find athabascaite
Classic worldwide localities
- Athabasca region, Saskatchewan, Canada
- Tien Shan, Uzbekistan
- Hope's Nose, Devon, England
Field-hunting tip
Look in hydrothermal vein deposits country — that is the host setting where athabascaite typically forms. If you start seeing klockmannite, umangite, clausthalite in float, you are in the right ground. Field specimens usually show a massive, anhedral grains habit, so train your eye for that shape before scanning the outcrop.





