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 4, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: black.
- 3Read the lusterHold the specimen under a strong light. Luster: metallic.
- 4Match the color rangeCompare against the expected color range: steel gray.
- 5Look at form & habitCrystal system: tetragonal. Typical habit: aggregates.
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
- Cu₂(Sb,Tl)
- Mohs hardness
- 4
- Density
- 8.42 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Tetragonal
- Crystal habit
- Aggregates
- Cleavage
- One direction
- Rarity
- Rare
- Uses
- Collector
- Host rock
- As fine-grained aggregates in a vein of ussingite cutting sodalite syenite (Ilímaussaq intrusion, Greenland); in sulfide veins in metamorphic siliceous dolostone (Långsjön, Sweden)
Where rockhounds find cuprostibite
Classic worldwide localities
- Franklin, Sussex Co., New Jersey, USA
- Southern Greenland, from Mt. Nákâlâq (type locality), northwest of Taseq Lake
- Långsjön, at Långban, and in the Getberg mine, near Långban, Värmland, Sweden
Field-hunting tip
Where it forms: As fine-grained aggregates in a vein of ussingite cutting sodalite syenite (Ilímaussaq intrusion, Greenland); in sulfide veins in metamorphic siliceous dolostone (Långsjön, Sweden). If you start seeing löllingite, antimonian silver, chalcopyrite in float, you are in the right ground. Typical habit: aggregates. Train your eye for that shape before scanning the outcrop.








