Laitakarite is a rare bismuth selenide sulfide mineral typically found in hydrothermal vein deposits. It is best identified by its metallic, lead-gray color and perfect basal cleavage, often appearing as small lamellar or tabular crystals.
Is this laitakarite?
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 laitakarite with a known reference. Laitakarite 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. Laitakarite leaves a gray streak.
- 3Read the lusterHold the specimen under a strong light. Laitakarite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: lead-gray, tin-white.
- 5Look at form & habitCrystal system: trigonal. Typical habit: lamellar or tabular crystals, massive.
Often confused with
Laitakarite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside laitakarite
Minerals reported to co-occur with laitakarite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Bi₄Se₂S
- Mohs hardness
- 2
- Density
- 8.06 g/cm³
- Streak
- Gray
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Trigonal
- Crystal habit
- Lamellar or Tabular Crystals, Massive
- Cleavage
- Perfect Basal
- Rarity
- Rare
- Uses
- Collector, Scientific Research
- Host rock
- Hydrothermal Veins
- Typical price
- $50-300 per specimen
Where rockhounds find laitakarite
Classic worldwide localities
- Laitakari, Finland
- Sweden
- China
- Kazakhstan
Field-hunting tip
Look in hydrothermal veins country, the host setting where laitakarite typically forms. If you start seeing bismuthinite, chalcopyrite, pyrite in float, you are in the right ground. Field specimens usually show a lamellar or tabular crystals, massive habit, so train your eye for that shape before scanning the outcrop.





