Radhakrishnaite is an extremely rare lead-silver-copper telluride mineral found primarily in epithermal gold deposits. It usually occurs as microscopic grains associated with other tellurides, making it difficult to identify without laboratory analysis like EDS or X-ray diffraction.
Is this radhakrishnaite?
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 radhakrishnaite with a known reference. Radhakrishnaite sits at Mohs 2-3 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Radhakrishnaite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Radhakrishnaite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: white, gray.
- 5Look at form & habitCrystal system: tetragonal. Typical habit: anhedral grains, interstitial masses.
Often confused with
Radhakrishnaite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside radhakrishnaite
Minerals reported to co-occur with radhakrishnaite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- PbTe₃(Ag,Cu)₂
- Mohs hardness
- 2-3
- Density
- 9.4-9.6 g/cm³
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Tetragonal
- Crystal habit
- Anhedral Grains, Interstitial Masses
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Epithermal Gold-telluride Deposits
- Typical price
- expensive due to extreme rarity
Where rockhounds find radhakrishnaite
Classic worldwide localities
- Kochbulak gold deposit, Uzbekistan
Field-hunting tip
Look in epithermal gold-telluride deposits country — that is the host setting where radhakrishnaite typically forms. If you start seeing gold, altaite, tetradymite in float, you are in the right ground. Field specimens usually show a anhedral grains, interstitial masses habit, so train your eye for that shape before scanning the outcrop.





