Inaglyite is a rare lead copper telluride mineral found primarily in epithermal gold-telluride deposits. It typically occurs as small, metallic inclusions within larger ore minerals and is prized by advanced micromount collectors due to its scarcity.
Is this inaglyite?
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 inaglyite with a known reference. Inaglyite sits at Mohs 2.5-3, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Inaglyite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Inaglyite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: lead-gray, steel-gray.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: anhedral to subhedral grains.
Often confused with
Inaglyite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside inaglyite
Minerals reported to co-occur with inaglyite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- PbCu₃Ir₈S₁₆
- Mohs hardness
- 2.5-3
- Density
- 8.8-9.2 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Hexagonal
- Crystal habit
- Anhedral to Subhedral Grains
- Cleavage
- In Two Directions
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Epithermal Gold Deposits
Where rockhounds find inaglyite
Classic worldwide localities
- Inagli massif, Yakutia, Russia
Field-hunting tip
Look in epithermal gold deposits country, the host setting where inaglyite typically forms. If you start seeing altaite, gold, pyrite in float, you are in the right ground. Field specimens usually show a anhedral to subhedral grains habit, so train your eye for that shape before scanning the outcrop.






