Ferronickelplatinum is a rare platinum-group mineral typically occurring as microscopic grains within heavy mineral concentrates or ultramafic complexes. It is visually indistinguishable from native platinum without advanced microprobe or X-ray diffraction analysis and is primarily sought by advanced mineral collectors and researchers.

Hardness
5
Mohs
Luster
Metallic
Streak
Gray
Transparency
Opaque

Is this ferronickelplatinum?

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 ferronickelplatinum with a known reference. Ferronickelplatinum sits at Mohs 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: gray.
  • 3
    Read the luster
    Hold the specimen under a strong light. Luster: metallic.
  • 4
    Match the color range
    Compare against the expected color range: silver white.
  • 5
    Look at form & habit
    Crystal system: tetragonal. Typical habit: microscopic crystals.

Often confused with

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

Often found alongside ferronickelplatinum

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

All properties

Chemical formula
Pt₂FeNi
Mohs hardness
5
Density
15.39 g/cm³
Streak
Gray
Luster
Metallic
Transparency
Opaque
Crystal system
Tetragonal
Crystal habit
Microscopic crystals
Cleavage
None
Rarity
Rare
Uses
Scientific study, Collector
Host rock
In the heavy fraction of Quaternary alluvial deposits associated with ultramafics from an ophiolite belt (Northern Pekul’nei River, Russia)

Where rockhounds find ferronickelplatinum

Classic worldwide localities

  • Goodnews Bay, Alaska, USA
  • Placer of the Northern Pekul’nei River, Pekul’nei Range, eastern Chukot Peninsula, Russia (type locality)
  • Naran massif, western Mongolia

Field-hunting tip

Where it forms: In the heavy fraction of Quaternary alluvial deposits associated with ultramafics from an ophiolite belt (Northern Pekul’nei River, Russia). If you start seeing isoferroplatinum, tetraferroplatinum, rutheniridosmine in float, you are in the right ground. Typical habit: microscopic crystals. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify ferronickelplatinum?+
Mohs hardness is 5. Luster: metallic. The streak is gray. Common colors include silver white.
Where is ferronickelplatinum found?+
Notable localities include Goodnews Bay, Alaska, USA; Placer of the Northern Pekul’nei River, Pekul’nei Range, eastern Chukot Peninsula, Russia (type locality); Naran massif, western Mongolia.
Is ferronickelplatinum safe to handle?+
Ferronickelplatinum contains nickel. Wash your hands afterwards, never grind or breathe the dust, and store it apart from specimens you handle often.
What rocks look like ferronickelplatinum?+
Ferronickelplatinum is most often confused with Platinum, Isoferroplatinum, Tulameenite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with ferronickelplatinum?+
Ferronickelplatinum commonly co-occurs with Isoferroplatinum, Tetraferroplatinum, Rutheniridosmine, Laurite, Irarsite, Cooperite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does ferronickelplatinum form in?+
Where it forms: In the heavy fraction of Quaternary alluvial deposits associated with ultramafics from an ophiolite belt (Northern Pekul’nei River, Russia). Working float back to the host body is the standard way to chase a fresh occurrence.
What is ferronickelplatinum used for?+
Ferronickelplatinum is used in scientific study, collector.

Find ferronickelplatinum on the map

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