Pääkkönenite is a rare antimony arsenic sulfide mineral originally discovered in the Seinäjoki antimony deposits of Finland. It typically forms metallic, gray, acicular crystals or fibrous aggregates that are visually similar to stibnite but distinguishable by its distinct composition and crystal system.
Is this pääkkönenite?
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 pääkkönenite with a known reference. Pääkkönenite sits at Mohs ~2, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: gray with a brownish tint.
- 3Read the lusterHold the specimen under a strong light. Luster: metallic.
- 4Match the color rangeCompare against the expected color range: gray.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: irregular grains.
Often confused with
Pääkkönenite vs. its common look-alikes, and how to tell them apart in the field.

How to tell apart: Streak differs, so Pääkkönenite leaves gray with a brownish tint, Stibnite leaves lead-gray.

How to tell apart: Arsenopyrite is the harder of the two (Mohs 5.5-6 vs. ~2); streak differs, so Pääkkönenite leaves gray with a brownish tint, Arsenopyrite leaves black.
Often found alongside pääkkönenite
Minerals reported to co-occur with pääkkönenite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Sb₂AsS₂
- Mohs hardness
- ~2
- Density
- 5.21 g/cm³
- Colors
- Streak
- Gray with a brownish tint
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Monoclinic
- Crystal habit
- Irregular grains
- Cleavage
- In one direction
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In hydrothermal mineral deposits with other Sb–As-bearing minerals
Where rockhounds find pääkkönenite
Classic worldwide localities
- Kalliosalo deposit, Seinäjoki region, Finland (type locality)
- Příbram, Czech Republic
- Hemlo gold deposit, Hemlo, Ontario, Canada
Field-hunting tip
Where it forms: In hydrothermal mineral deposits with other Sb–As-bearing minerals. If you start seeing arsenopyrite, arsenic, löllingite in float, you are in the right ground. Typical habit: irregular grains. Train your eye for that shape before scanning the outcrop.




