Henryite is a rare copper-silver telluride mineral typically found as microscopic inclusions within other telluride ores in epithermal gold deposits. It is best identified through polished section analysis using reflected light microscopy where it displays a distinct creamy white to pale yellow color. Specimens are primarily sourced from the telluride-rich mining districts of Colorado.
Is this henryite?
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 henryite with a known reference. Henryite sits at Mohs 2.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Henryite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Henryite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: white, pale yellow.
- 5Look at form & habitCrystal system: tetragonal. Typical habit: anhedral grains, inclusions.
Often confused with
Henryite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside henryite
Minerals reported to co-occur with henryite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Cu₄Ag₃Te₄
- Mohs hardness
- 2.5
- Density
- 8.55 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Tetragonal
- Crystal habit
- Anhedral Grains, Inclusions
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Epithermal Gold-telluride Veins
- Typical price
- $50-300 per micro-mount or small specimen
Where rockhounds find henryite
Classic worldwide localities
- Good Hope mine, Colorado, USA
- Sacarmento mine, Colorado, USA
- Empress Josephine mine, Colorado, USA
Field-hunting tip
Look in epithermal gold-telluride veins country — that is the host setting where henryite typically forms. If you start seeing petzite, hessite, rickardite in float, you are in the right ground. Field specimens usually show a anhedral grains, inclusions habit, so train your eye for that shape before scanning the outcrop.





