Colusite is a rare copper-vanadium-arsenic sulfosalt often found as fine-grained masses within hydrothermal copper ore deposits. It is best identified in polished section under reflected light by its distinctive bronze-brown color and association with other complex sulfides.
Is this colusite?
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 colusite with a known reference. Colusite sits at Mohs 3-4 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Colusite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Colusite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: bronze-brown, dark gray, brass-yellow.
- 5Look at form & habitCrystal system: cubic. Typical habit: massive, granular, rarely as small tetrahedral crystals.
Often confused with
Colusite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside colusite
Minerals reported to co-occur with colusite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Cu₂₆V₂As₆S₃₂
- Mohs hardness
- 3-4
- Density
- 4.5-4.6 g/cm³
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Cubic
- Crystal habit
- Massive, Granular, Rarely as Small Tetrahedral Crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector, Scientific Research
- Host rock
- Hydrothermal Copper-arsenic Deposits
- Typical price
- $20-150 depending on size and association
Where rockhounds find colusite
Classic worldwide localities
- Butte, Montana (USA)
- Bor, Serbia
- Tsumeb, Namibia
- Srednogorie, Bulgaria
Field-hunting tip
Look in hydrothermal copper-arsenic deposits country — that is the host setting where colusite typically forms. If you start seeing enargite, tennantite, pyrite in float, you are in the right ground. Field specimens usually show a massive, granular, rarely as small tetrahedral crystals habit, so train your eye for that shape before scanning the outcrop.





