Lindströmite is a rare lead-copper-bismuth sulfosalt that typically occurs as slender, acicular crystals or fibrous masses within hydrothermal deposits. It is often indistinguishable from bismuthinite in hand samples, typically requiring laboratory methods like X-ray diffraction or microprobe analysis for positive identification.

Hardness
3-3.5
Mohs
Luster
Metallic
Streak
Black
Transparency
Opaque

Is this lindströmite?

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 lindströmite with a known reference. Lindströmite sits at Mohs 3-3.5, softer than the next harder reference, harder than the previous one.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Streak: black.
  • 3
    Read the luster
    Hold the specimen under a strong light. Luster: metallic.
  • 4
    Match the color range
    Compare against the expected color range: gray, tin white.
  • 5
    Look at form & habit
    Crystal system: orthorhombic. Typical habit: prismatic, striated.

Often confused with

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

Often found alongside lindströmite

Minerals reported to co-occur with lindströmite. Spotting these in float or country rock is a strong cue you are in the right ground.

All properties

Chemical formula
Cu₃Pb₃Bi₇S₁₅
Mohs hardness
3-3.5
Density
7.01 g/cm³
Streak
Black
Luster
Metallic
Transparency
Opaque
Crystal system
Orthorhombic
Crystal habit
Prismatic, striated
Cleavage
Good on {100} and {010}; also on {230}
Rarity
Rare
Uses
Collector, Research
Host rock
Of hydrothermal origin

Where rockhounds find lindströmite

Classic worldwide localities

  • Beaver Mountains, near Milford, Beaver Co., Utah, and at Manhattan, Nye Co., Nevada, USA
  • Gladhammar, Kalmar, Sweden (type locality)
  • Beresovsk district, near Yekaterinburg (Sverdlovsk), Middle Ural Mountains, and at Inkur, Transbaikal, Russia
  • Baia Borşa, Baia Mare (Nagybánya), Romania
  • Spissko-Gemerske Rudohorie Mountains, Slovakia
  • Loch Shin monzogranite, near Lairg, Scotland

Field-hunting tip

Where it forms: Of hydrothermal origin. If you start seeing krupkaite, bismuth in float, you are in the right ground. Typical habit: prismatic, striated. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify lindströmite?+
Mohs hardness is 3-3.5. Luster: metallic. The streak is black. Common colors include gray, tin white.
Where is lindströmite found?+
Notable localities include Beaver Mountains, near Milford, Beaver Co., Utah, and at Manhattan, Nye Co., Nevada, USA; Gladhammar, Kalmar, Sweden (type locality); Beresovsk district, near Yekaterinburg (Sverdlovsk), Middle Ural Mountains, and at Inkur, Transbaikal, Russia; Baia Borşa, Baia Mare (Nagybánya), Romania; Spissko-Gemerske Rudohorie Mountains, Slovakia.
Is lindströmite safe to handle?+
Lindströmite contains copper and lead. Contains lead and bismuth; handle with care and wash hands thoroughly after handling. Do not ingest or inhale dust.
What rocks look like lindströmite?+
Lindströmite is most often confused with Aikinite, Bismuthinite, Emplectite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with lindströmite?+
Lindströmite commonly co-occurs with Krupkaite, Bismuth. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does lindströmite form in?+
Where it forms: Of hydrothermal origin. Working float back to the host body is the standard way to chase a fresh occurrence.
What is lindströmite used for?+
Lindströmite is used in collector, research.

Find lindströmite on the map

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