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, 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.



