Stumpflite is a rare platinum-antimonide mineral typically found as microscopic grains within massive sulfide deposits in ultramafic rocks. It is usually identified through polished section microscopy in laboratory settings due to its small crystal size and affinity for other platinum-group minerals.
Is this stumpflite?
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 stumpflite with a known reference. Stumpflite sits at Mohs 3 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Stumpflite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Stumpflite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: white, gray.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: grains, inclusions.
Often confused with
Stumpflite vs. its common look-alikes — and how to tell them apart in the field.
How to tell apart: Geversite is the harder of the two (Mohs 5.5 vs. 3).

How to tell apart: Genkinite is the harder of the two (Mohs 4 vs. 3).

How to tell apart: Sperrylite is the harder of the two (Mohs 6-7 vs. 3).
Often found alongside stumpflite
Minerals reported to co-occur with stumpflite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pt(Sb,Bi)
- Mohs hardness
- 3
- Density
- 8.55 g/cm³
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Hexagonal
- Crystal habit
- Grains, Inclusions
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Ultramafic Igneous Complexes
- Typical price
- $100-500 per specimen
Where rockhounds find stumpflite
Classic worldwide localities
- Driekop mine, South Africa
- Onverwacht pipe, South Africa
- Stillwater complex, USA
- Norilsk, Russia
Field-hunting tip
Look in ultramafic igneous complexes country — that is the host setting where stumpflite typically forms. If you start seeing platinum, cooperite, braggite in float, you are in the right ground. Field specimens usually show a grains, inclusions habit, so train your eye for that shape before scanning the outcrop.





