Pentlandite is the primary source of nickel and typically occurs in granular or massive aggregates within sulfide ore bodies. It is easily recognized by its distinct bronze-yellow color and tendency to be found in close association with magnetic pyrrhotite. Collectors often prize specimens from the major nickel-copper mining districts like Sudbury.

Hardness
3.5-4
Mohs
Luster
Metallic
Streak
Light Bronze-brown
Transparency
Opaque

Is this pentlandite?

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 pentlandite with a known reference. Pentlandite sits at Mohs 3.5-4 — softer than the next harder reference, harder than the previous one.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Pentlandite leaves a light bronze-brown streak.
  • 3
    Read the luster
    Hold the specimen under a strong light. Pentlandite typically shows a metallic luster.
  • 4
    Match the color range
    Compare against the expected color range: bronze-yellow, brownish-yellow.
  • 5
    Look at form & habit
    Crystal system: cubic. Typical habit: granular, massive, rarely as octahedral crystals.

Often confused with

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

Often found alongside pentlandite

Minerals reported to co-occur with pentlandite. Spotting these in float or country rock is a strong cue you are in the right ground.

All properties

Chemical formula
(Fe,Ni)₉S₈
Mohs hardness
3.5-4
Density
4.6-5.0 g/cm³
Streak
Light Bronze-brown
Luster
Metallic
Transparency
Opaque
Crystal system
Cubic
Crystal habit
Granular, Massive, Rarely as Octahedral Crystals
Cleavage
None
Rarity
Common
Uses
Industrial, Ore of Nickel, Collector
Host rock
Mafic and Ultramafic Igneous Rocks
Typical price
$10-60 for small mineral specimens

Where rockhounds find pentlandite

Classic worldwide localities

  • Sudbury, Ontario, Canada
  • Norilsk, Russia
  • Bushveld Complex, South Africa
  • Kambalda, Australia
  • Voisey's Bay, Canada

Field-hunting tip

Look in mafic and ultramafic igneous rocks country — that is the host setting where pentlandite typically forms. If you start seeing pyrrhotite, chalcopyrite, magnetite in float, you are in the right ground. Field specimens usually show a granular, massive, rarely as octahedral crystals habit, so train your eye for that shape before scanning the outcrop.

Common questions

How do you identify pentlandite?+
Mohs hardness is 3.5-4. It typically shows a metallic luster. The streak is light bronze-brown. Common colors include bronze-yellow, brownish-yellow.
Where is pentlandite found?+
Notable localities include Sudbury, Ontario, Canada; Norilsk, Russia; Bushveld Complex, South Africa; Kambalda, Australia; Voisey's Bay, Canada.
How much is pentlandite worth?+
Typical asking prices fall in the range of $10-60 for small mineral specimens. Quality, size, and provenance can move individual specimens well outside that range.
What rocks look like pentlandite?+
Pentlandite is most often confused with Pyrrhotite, Chalcopyrite, Pyrite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with pentlandite?+
Pentlandite commonly co-occurs with Pyrrhotite, Chalcopyrite, Magnetite, Cubanite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does pentlandite form in?+
Pentlandite typically forms in mafic and ultramafic igneous rocks. Working float back to the host body is the standard way to chase a fresh occurrence.
What is pentlandite used for?+
Pentlandite is used in industrial, ore of nickel, collector.

Find pentlandite on the map

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