Isoferroplatinum is a rare platinum-iron alloy typically occurring as small metallic grains within mafic and ultramafic igneous complexes. It is distinguished from native platinum by its high iron content and distinct optical properties under reflected light, often requiring microprobe analysis for positive identification.

Hardness
5
Mohs
Luster
Metallic
Streak
Grayish-black
Transparency
Opaque

Is this isoferroplatinum?

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 isoferroplatinum with a known reference. Isoferroplatinum 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: grayish-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: gray, dark gray.
  • 5
    Look at form & habit
    Crystal system: cubic. Typical habit: anhedral grains, nuggets, rounded inclusions in chromite.

Often confused with

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

Often found alongside isoferroplatinum

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

All properties

Chemical formula
Pt₃Fe
Mohs hardness
5
Density
16.5 g/cm³
Streak
Grayish-black
Luster
Metallic
Transparency
Opaque
Crystal system
Cubic
Crystal habit
Anhedral grains, nuggets, rounded inclusions in chromite
Cleavage
None
Rarity
Rare
Uses
Collector, Scientific reference
Host rock
In Pt–Fe and Cu–Ni sulfide deposits in ultramafic rocks, also in chromatites, and placers derived from them

Where rockhounds find isoferroplatinum

Classic worldwide localities

  • Stillwater complex, Montana, and at Fox Gulch, Goodnews Bay, Alaska, USA
  • Tulameen (type locality) and Similkameen Rivers, British Columbia, Canada
  • Department of Chocó, Cauca, Colombia
  • Inagli and Konder massifs, Aldan Shield, Sakha, Russia
  • Noril’sk region, western Siberia, Russia
  • Gusevogorskii pluton and the Kytlym and Uktus complexes, Ural Mountains, Russia

Field-hunting tip

Where it forms: In Pt–Fe and Cu–Ni sulfide deposits in ultramafic rocks, also in chromatites, and placers derived from them. If you start seeing platinum, iridium, osmium in float, you are in the right ground. Typical habit: anhedral grains, nuggets, rounded inclusions in chromite. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify isoferroplatinum?+
Mohs hardness is 5. Luster: metallic. The streak is grayish-black. Common colors include gray, dark gray.
Where is isoferroplatinum found?+
Notable localities include Stillwater complex, Montana, and at Fox Gulch, Goodnews Bay, Alaska, USA; Tulameen (type locality) and Similkameen Rivers, British Columbia, Canada; Department of Chocó, Cauca, Colombia; Inagli and Konder massifs, Aldan Shield, Sakha, Russia; Noril’sk region, western Siberia, Russia.
What rocks look like isoferroplatinum?+
Isoferroplatinum is most often confused with Native Platinum, Sperrylite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with isoferroplatinum?+
Isoferroplatinum commonly co-occurs with Platinum, Iridium, Osmium, Pt–Fe alloy, Braggite, Sperrylite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does isoferroplatinum form in?+
Where it forms: In Pt–Fe and Cu–Ni sulfide deposits in ultramafic rocks, also in chromatites, and placers derived from them. Working float back to the host body is the standard way to chase a fresh occurrence.
What is isoferroplatinum used for?+
Isoferroplatinum is used in collector, scientific reference.

Find isoferroplatinum on the map

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