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.

Hardness
4.5-5
Mohs
Luster
Metallic
Streak
Black
Transparency
Opaque

Is this lapieite?

5-step field check

Run through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.

  • 1
    Test the hardness
    Try to scratch lapieite with a known reference. Lapieite sits at Mohs 4.5-5, softer than the next harder reference, harder than the previous one.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Streak: black.
  • 3
    Read the luster
    Hold the specimen under a strong light. Luster: metallic.
  • 4
    Match the color range
    Compare against the expected color range: steel gray.
  • 5
    Look at form & habit
    Crystal system: orthorhombic. Typical habit: anhedral grains.

Often confused with

Lapieite vs. its common look-alikes, and how to tell them apart in the field.

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
4.5-5
Density
4.966 g/cm³
Streak
Black
Luster
Metallic
Transparency
Opaque
Crystal system
Orthorhombic
Crystal habit
Anhedral grains
Cleavage
Distinct on {100}
Rarity
Rare
Uses
Collector
Host rock
In a highly altered and mineralized glacial erratic (Lapie River, Canada)

Where rockhounds find lapieite

Classic worldwide localities

  • Confluence of Glacier Creek and the Lapie River, St. Cyr Ranges, Yukon Territory, Canada (type locality)
  • Tyrnyauz deposit, left bank of the Baksan River Valley, northern Caucasus Mountains, Russia
  • Grüne gold mine, Schutzbach, 15 km southwest of Siegen, North-Rhine-Westphalia, Germany

Field-hunting tip

Where it forms: In a highly altered and mineralized glacial erratic (Lapie River, Canada). If you start seeing nickelian pyrite, gersdorffite, polydymite in float, you are in the right ground. Typical habit: anhedral grains. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify lapieite?+
Mohs hardness is 4.5-5. Luster: metallic. The streak is black. Common colors include steel gray.
Where is lapieite found?+
Notable localities include Confluence of Glacier Creek and the Lapie River, St. Cyr Ranges, Yukon Territory, Canada (type locality); Tyrnyauz deposit, left bank of the Baksan River Valley, northern Caucasus Mountains, Russia; Grüne gold mine, Schutzbach, 15 km southwest of Siegen, North-Rhine-Westphalia, Germany.
Is lapieite safe to handle?+
Lapieite contains antimony, copper and nickel. Contains nickel, copper, and antimony. Handle with care, avoid inhalation of dust, and wash hands thoroughly after handling.
What rocks look like lapieite?+
Lapieite is most often confused with Ullmannite, Gersdorffite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with lapieite?+
Lapieite commonly co-occurs with Nickelian pyrite, Gersdorffite, Polydymite, Millerite, Marcasite, Tetrahedrite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does lapieite form in?+
Where it forms: In a highly altered and mineralized glacial erratic (Lapie River, Canada). Working float back to the host body is the standard way to chase a fresh occurrence.
What is lapieite used for?+
Lapieite is used in collector.

Find lapieite on the map

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