Shandite is a rare nickel-lead sulfide mineral that typically presents as bronze or brassy metallic grains. It is primarily found in hydrothermal deposits, often associated with other base metal sulfides in specialized geological settings.
Is this shandite?
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 shandite with a known reference. Shandite sits at Mohs 3.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Shandite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Shandite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: bronze, pale brass-yellow.
- 5Look at form & habitCrystal system: trigonal. Typical habit: tabular crystals, massive, granular.
Often confused with
Shandite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside shandite
Minerals reported to co-occur with shandite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pb₂Ni₃S₂
- Mohs hardness
- 3.5
- Density
- 7.5 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Trigonal
- Crystal habit
- Tabular Crystals, Massive, Granular
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Veins
- Typical price
- $100-500 depending on specimen size and quality
Where rockhounds find shandite
Classic worldwide localities
- Gladhammar, Sweden
- Potarite locality, Guyana
Field-hunting tip
Look in hydrothermal veins country — that is the host setting where shandite typically forms. If you start seeing galena, bornite, chalcopyrite in float, you are in the right ground. Field specimens usually show a tabular crystals, massive, granular habit, so train your eye for that shape before scanning the outcrop.





