Cuprostibite is an extremely rare copper antimony mineral typically found as small, non-descript grains within alkaline igneous rocks. It is primarily identified in lab settings due to its subtle metallic appearance and association with exotic minerals in the Ilimaussaq complex.
Is this cuprostibite?
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 cuprostibite with a known reference. Cuprostibite sits at Mohs 3.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Cuprostibite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Cuprostibite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: dark gray, bronze-like, light red.
- 5Look at form & habitCrystal system: trigonal. Typical habit: massive, anhedral grains, interstitial.
Often confused with
Cuprostibite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside cuprostibite
Minerals reported to co-occur with cuprostibite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Cu₂Sb
- Mohs hardness
- 3.5
- Density
- 8.84 g/cm³
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Trigonal
- Crystal habit
- Massive, Anhedral Grains, Interstitial
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Agpaitic Nepheline Syenite Pegmatites
- Typical price
- $50-300 per micro-mount or small specimen
Where rockhounds find cuprostibite
Classic worldwide localities
- Ilimaussaq complex, Greenland
- Yukon, Canada
Field-hunting tip
Look in agpaitic nepheline syenite pegmatites country — that is the host setting where cuprostibite typically forms. If you start seeing djerfisherite, villiaumite, sodalite in float, you are in the right ground. Field specimens usually show a massive, anhedral grains, interstitial habit, so train your eye for that shape before scanning the outcrop.






