Seinäjokite is a rare antimony-bearing member of the löllingite group characterized by its high density and metallic luster. It is typically found in small, massive grains within hydrothermal veins and often requires laboratory analysis for definitive identification due to its similarity to other iron-antimonide minerals.
Is this seinäjokite?
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 seinäjokite with a known reference. Seinäjokite 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. Seinäjokite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Seinäjokite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: tin-white, silver-white.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: massive, anhedral grains.
Often confused with
Seinäjokite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside seinäjokite
Minerals reported to co-occur with seinäjokite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- FeSb₂
- Mohs hardness
- 5-6
- Density
- 7.52 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Orthorhombic
- Crystal habit
- Massive, Anhedral Grains
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Veins, Metamorphosed Ore Deposits
- Typical price
- $50-200 per specimen
Where rockhounds find seinäjokite
Classic worldwide localities
- Seinäjoki, Finland
- Ivigtut, Greenland
- Broken Hill, Australia
Field-hunting tip
Look in hydrothermal veins, metamorphosed ore deposits country — that is the host setting where seinäjokite typically forms. If you start seeing stibnite, pyrrhotite, arsenopyrite in float, you are in the right ground. Field specimens usually show a massive, anhedral grains habit, so train your eye for that shape before scanning the outcrop.





