Shadlunite is a rare lead-bearing member of the pentlandite group typically found within copper-nickel sulfide ore bodies. It occurs as massive, brass-yellow to bronze aggregates that are nearly impossible to distinguish from similar sulfides without laboratory analysis like X-ray diffraction.
Is this shadlunite?
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 shadlunite with a known reference. Shadlunite sits at Mohs 3.5-4, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Shadlunite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Shadlunite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: brass-yellow, bronze.
- 5Look at form & habitCrystal system: cubic. Typical habit: massive, granular aggregates.
Often confused with
Shadlunite vs. its common look-alikes, and how to tell them apart in the field.

How to tell apart: Streak differs, so Shadlunite leaves black, Pentlandite leaves light bronze-brown.

How to tell apart: Streak differs, so Shadlunite leaves black, Chalcopyrite leaves greenish-black.

Often found alongside shadlunite
Minerals reported to co-occur with shadlunite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Pb,Cd)(Fe,Cu)₈S₈
- Mohs hardness
- 3.5-4
- Density
- 4.95-5.05 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Cubic
- Crystal habit
- Massive, Granular Aggregates
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Copper-nickel Sulfide Ore Deposits
- Typical price
- $50-300 per specimen
Where rockhounds find shadlunite
Classic worldwide localities
- Talnakh deposit, Russia
- Norilsk, Russia
Field-hunting tip
Look in copper-nickel sulfide ore deposits country, the host setting where shadlunite typically forms. If you start seeing pentlandite, chalcopyrite, cubanite in float, you are in the right ground. Field specimens usually show a massive, granular aggregates habit, so train your eye for that shape before scanning the outcrop.

