Konderite is an extremely rare platinum-group mineral typically found in the heavy mineral concentrates of ultramafic complexes. Collectors usually identify it through laboratory analysis as it appears as tiny, inconspicuous metallic grains alongside other platinum-group minerals.
Is this konderite?
5-step field checkRun through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.
- 1Test the hardnessTry to scratch konderite with a known reference. Konderite sits at Mohs 5.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: black.
- 3Read the lusterHold the specimen under a strong light. Luster: metallic.
- 4Match the color rangeCompare against the expected color range: steel gray.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: microscopic crystals.
Often confused with
Konderite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside konderite
Minerals reported to co-occur with konderite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- PbCu₃Rh₈S₁₆
- Mohs hardness
- 5.5
- Density
- 6.12 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Hexagonal
- Crystal habit
- Microscopic crystals
- Cleavage
- In two directions, “average”
- Rarity
- Rare
- Uses
- Collector
- Host rock
- As inclusions in a Pt–Fe alloy from an alkalic ultramafic massif
Where rockhounds find konderite
Classic worldwide localities
- Konder massif, Aldan Shield, Sakha, Russia (type locality)
Field-hunting tip
Where it forms: As inclusions in a Pt–Fe alloy from an alkalic ultramafic massif. If you start seeing pt–fe alloy, erlichmanite in float, you are in the right ground. Typical habit: microscopic crystals. Train your eye for that shape before scanning the outcrop.




