Gudmundite is a relatively uncommon iron antimony sulfide that typically appears as metallic, steel-gray masses. It is most easily identified in laboratory settings due to its striking resemblance to arsenopyrite, though it is often found in antimony-rich ore deposits rather than simple arsenic veins.
Is this gudmundite?
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 gudmundite with a known reference. Gudmundite sits at Mohs ~5-6, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: grayish black.
- 3Read the lusterHold the specimen under a strong light. Luster: metallic.
- 4Match the color rangeCompare against the expected color range: silvery white, steel gray.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: crystalline, massive.
Often confused with
Gudmundite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside gudmundite
Minerals reported to co-occur with gudmundite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- FeSbS
- Mohs hardness
- ~5-6
- Density
- 6.72 g/cm³
- Colors
- Streak
- Grayish black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Monoclinic
- Crystal habit
- Crystalline, massive
- Cleavage
- None
- Rarity
- Uncommon
- Uses
- Collector, Scientific research
- Host rock
- A late-stage hydrothermal mineral formed in sulfide deposits
Where rockhounds find gudmundite
Classic worldwide localities
- Gudmundstorp, 3 km north of Sala, Västmanland (type locality), Sweden
- Boliden, Holmtjärn, Malånäs, Tunaberg, and in the Vena mines, near Askersund, Örebro, Sweden
- Kalliolampi, near Nurma, Finland
- Sulitjelma, Norway
- Waldsassen, Bavaria, Germany
- Salsigne mine, 15 km north of Carcassone, Aude, France
Field-hunting tip
Where it forms: A late-stage hydrothermal mineral formed in sulfide deposits. If you start seeing pyrite, pyrrhotite, chalcopyrite in float, you are in the right ground. Typical habit: crystalline, massive. Train your eye for that shape before scanning the outcrop.








