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
4.5
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 4.5 — softer than the next harder reference, harder than the previous one.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Isoferroplatinum leaves a grayish-black streak.
  • 3
    Read the luster
    Hold the specimen under a strong light. Isoferroplatinum typically shows a metallic luster.
  • 4
    Match the color range
    Compare against the expected color range: silver-white, light steel-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
4.5
Density
17.4-18.3 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
Ultramafic Igneous Rocks
Typical price
$50-300 per specimen

Where rockhounds find isoferroplatinum

Classic worldwide localities

  • Stillwater Complex, USA
  • Bushveld Complex, South Africa
  • Ural Mountains, Russia
  • Tulameen Complex, Canada

Field-hunting tip

Look in ultramafic igneous rocks country — that is the host setting where isoferroplatinum typically forms. If you start seeing chromite, olivine, pyroxene in float, you are in the right ground. Field specimens usually show a anhedral grains, nuggets, rounded inclusions in chromite habit, so train your eye for that shape before scanning the outcrop.

Common questions

How do you identify isoferroplatinum?+
Mohs hardness is 4.5. It typically shows a metallic luster. The streak is grayish-black. Common colors include silver-white, light steel-gray.
Where is isoferroplatinum found?+
Notable localities include Stillwater Complex, USA; Bushveld Complex, South Africa; Ural Mountains, Russia; Tulameen Complex, Canada.
How much is isoferroplatinum worth?+
Typical asking prices fall in the range of $50-300 per specimen. Quality, size, and provenance can move individual specimens well outside that range.
What rocks look like isoferroplatinum?+
Isoferroplatinum is most often confused with Platinum Nuggets, 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 chromite, olivine, pyroxene, magnetite, native platinum. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does isoferroplatinum form in?+
Isoferroplatinum typically forms in ultramafic igneous rocks. 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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