Lapieite is an exceptionally rare sulfosalt mineral primarily known from its type locality at the Lapie River in Yukon, Canada. It typically occurs as minute anhedral grains within complex sulfide-rich hydrothermal veins associated with other nickel and copper minerals.
Is this lapieite?
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 lapieite with a known reference. Lapieite sits at Mohs 3-3.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Lapieite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Lapieite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: steel-gray, black.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: anhedral grains.
Often confused with
Lapieite vs. its common look-alikes — and how to tell them apart in the field.

How to tell apart: Ullmannite is the harder of the two (Mohs 5-5.5 vs. 3-3.5).

How to tell apart: Gersdorffite is the harder of the two (Mohs 5.5 vs. 3-3.5); streak differs — Lapieite leaves black, Gersdorffite leaves grayish-black.
Often found alongside lapieite
Minerals reported to co-occur with lapieite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CuNiSbS₃
- Mohs hardness
- 3-3.5
- Density
- 5.68 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Orthorhombic
- Crystal habit
- Anhedral Grains
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Veins in Sedimentary Rocks
- Typical price
- $50-300 for rare micro-specimens
Where rockhounds find lapieite
Classic worldwide localities
- Lapie River, Yukon Territory, Canada
Field-hunting tip
Look in hydrothermal veins in sedimentary rocks country — that is the host setting where lapieite typically forms. If you start seeing chalcopyrite, pyrite, gersdorffite in float, you are in the right ground. Field specimens usually show a anhedral grains habit, so train your eye for that shape before scanning the outcrop.



