Goldfieldite is a rare tellurium-rich member of the tetrahedrite group, typically appearing as metallic, steel-gray to black tetrahedral crystals or massive aggregates. It is primarily found in epithermal gold-telluride deposits, often associated with other rare tellurium-bearing minerals and quartz.
Is this goldfieldite?
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 goldfieldite with a known reference. Goldfieldite sits at Mohs 3-3.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Goldfieldite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Goldfieldite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: steel-gray, iron-black.
- 5Look at form & habitCrystal system: cubic. Typical habit: tetrahedral crystals, massive, granular.
Often confused with
Goldfieldite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside goldfieldite
Minerals reported to co-occur with goldfieldite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Cu₁₂Te₄S₁₃
- Mohs hardness
- 3-3.5
- Density
- 5.3-5.5 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Cubic
- Crystal habit
- Tetrahedral Crystals, Massive, Granular
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector, Scientific Study
- Host rock
- Hydrothermal Veins
- Typical price
- $20-200 depending on specimen size and matrix quality
Where rockhounds find goldfieldite
Classic worldwide localities
- Goldfield, Nevada, USA
- Kawazu mine, Japan
- Moctezuma, Mexico
- Bajan, Romania
Field-hunting tip
Look in hydrothermal veins country — that is the host setting where goldfieldite typically forms. If you start seeing tellurides, pyrite, quartz in float, you are in the right ground. Field specimens usually show a tetrahedral crystals, massive, granular habit, so train your eye for that shape before scanning the outcrop.





