Telargpalite is a rare palladium-silver telluride typically found as microscopic grains within massive sulfide ores. It is primarily identified through electron microprobe analysis and reflection microscopy due to its extremely small grain size and scarcity in nature.
Is this telargpalite?
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 telargpalite with a known reference. Telargpalite sits at Mohs 2-2.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: black.
- 3Read the lusterHold the specimen under a strong light. Luster: metallic.
- 4Match the color rangeCompare against the expected color range: steel gray.
- 5Look at form & habitCrystal system: cubic. Typical habit: microscopic crystals.
Often confused with
Telargpalite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside telargpalite
Minerals reported to co-occur with telargpalite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Pd,Ag)₃Te
- Mohs hardness
- 2-2.5
- Density
- 7.375 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Cubic
- Crystal habit
- Microscopic crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector, Scientific research
- Host rock
- In metasomatically altered Cu–Ni sulfide ores (Talnakh area, Russia); in the layered ultramafic Stillwater complex (Nye, Montana, USA)
Where rockhounds find telargpalite
Classic worldwide localities
- Nye, Stillwater Co., Montana, USA
- Oktyabr mine, Talnakh area, Noril’sk region, western Siberia (type locality), and in the Nadezhda deposit, Lukkulaisvaara layered intrusion, Karelia, Russia
Field-hunting tip
Where it forms: In metasomatically altered Cu–Ni sulfide ores (Talnakh area, Russia); in the layered ultramafic Stillwater complex (Nye, Montana, USA). If you start seeing chalcopyrite, bornite, millerite in float, you are in the right ground. Typical habit: microscopic crystals. Train your eye for that shape before scanning the outcrop.








