Cubanite is a brass-yellow sulfide mineral that is typically found as a result of exsolution from chalcopyrite-pyrrhotite solid solutions. It is best identified by its distinct bronze-yellow color and its frequent occurrence as characteristic twinned bladed crystals in hydrothermal ore deposits.
Is this cubanite?
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 cubanite with a known reference. Cubanite sits at Mohs 3.5-4 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Cubanite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Cubanite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: brass-yellow, bronze-yellow.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: tabular crystals, massive, twinned blades.
Often confused with
Cubanite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside cubanite
Minerals reported to co-occur with cubanite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CuFe₂S₃
- Mohs hardness
- 3.5-4
- Density
- 4.07-4.18 g/cm³
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Orthorhombic
- Crystal habit
- Tabular Crystals, Massive, Twinned Blades
- Cleavage
- Poor
- Rarity
- Uncommon
- Uses
- Collector, Research
- Host rock
- Hydrothermal Sulfide Deposits, Igneous Mafic Rocks
- Typical price
- $15-100 per specimen
Where rockhounds find cubanite
Classic worldwide localities
- Mayarí, Cuba
- Sudbury, Ontario, Canada
- Morro Velho, Brazil
- Voisey's Bay, Canada
Field-hunting tip
Look in hydrothermal sulfide deposits, igneous mafic rocks country — that is the host setting where cubanite typically forms. If you start seeing chalcopyrite, pyrrhotite, pentlandite in float, you are in the right ground. Field specimens usually show a tabular crystals, massive, twinned blades habit, so train your eye for that shape before scanning the outcrop.



