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.

Hardness
2-3
Mohs
Luster
Metallic
Streak
Black
Transparency
Opaque

Is this pääkkönenite?

5-step field check

Run through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.

  • 1
    Test the hardness
    Try to scratch pääkkönenite with a known reference. Pääkkönenite sits at Mohs 2-3 — softer than the next harder reference, harder than the previous one.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Pääkkönenite leaves a black streak.
  • 3
    Read the luster
    Hold the specimen under a strong light. Pääkkönenite typically shows a metallic luster.
  • 4
    Match the color range
    Compare against the expected color range: lead-gray, silver-gray.
  • 5
    Look at form & habit
    Crystal system: monoclinic. Typical habit: acicular to prismatic crystals, often as fibrous or radial aggregates.

Often confused with

Pääkkönenite vs. its common look-alikes — and how to tell them apart in the field.

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
2-3
Density
6.83 g/cm³
Streak
Black
Luster
Metallic
Transparency
Opaque
Crystal system
Monoclinic
Crystal habit
Acicular to Prismatic Crystals, Often as Fibrous or Radial Aggregates
Cleavage
Perfect On {010}
Rarity
Rare
Uses
Collector
Host rock
Hydrothermal Antimony-arsenic Deposits
Typical price
$50-300 per specimen

Where rockhounds find pääkkönenite

Classic worldwide localities

  • Seinäjoki, Finland
  • Hemerdon Mine, England
  • Broken Hill, Australia

Field-hunting tip

Look in hydrothermal antimony-arsenic deposits country — that is the host setting where pääkkönenite typically forms. If you start seeing stibnite, arsenopyrite, löllingite in float, you are in the right ground. Field specimens usually show a acicular to prismatic crystals, often as fibrous or radial aggregates habit, so train your eye for that shape before scanning the outcrop.

Common questions

How do you identify pääkkönenite?+
Mohs hardness is 2-3. It typically shows a metallic luster. The streak is black. Common colors include lead-gray, silver-gray.
Where is pääkkönenite found?+
Notable localities include Seinäjoki, Finland; Hemerdon Mine, England; Broken Hill, Australia.
How much is pääkkönenite worth?+
Typical asking prices fall in the range of $50-300 per specimen. Quality, size, and provenance can move individual specimens well outside that range.
Is pääkkönenite safe to handle?+
It contains toxic constituents. Contains arsenic and antimony. Wash hands thoroughly after handling specimens and avoid inhaling dust when cleaning or trimming. Handle with care, avoid grinding or breathing dust, and store separately.
What rocks look like pääkkönenite?+
Pääkkönenite is most often confused with Stibnite, Arsenopyrite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with pääkkönenite?+
Pääkkönenite commonly co-occurs with Stibnite, Arsenopyrite, Löllingite, Quartz. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does pääkkönenite form in?+
Pääkkönenite typically forms in hydrothermal antimony-arsenic deposits. Working float back to the host body is the standard way to chase a fresh occurrence.
What is pääkkönenite used for?+
Pääkkönenite is used in collector.

Find pääkkönenite on the map

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