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, 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.





