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, so 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, 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.



