Galena specimen

Crystal & mineral guide

Galena

PbS

OreSulfideLead

Primary lead ore — perfect cubic cleavage and extreme density.

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About Galena

Galena's bright metallic cubes and perfect cleavage are textbook ore ID. Extremely dense and soft. Often silver-bearing — historically a major silver source as well as lead. Fresh surfaces darken with time.

Galena belongs in a crystal identifier workflow because photo cues — color zoning, crystal habit, and surface luster — combine with measurable traits like Mohs 2.5 and specific gravity 7.4–7.6. Use RockScan’s camera to get a first-pass ID, then confirm with the checklist below.

Galena properties

Mohs hardness2.5
Crystal systemCubic
LusterMetallic
ColorLead-gray
CompositionLead sulfide
FormationHydrothermal veins and Mississippi Valley-type deposits
OccurrenceUSA, Australia, China, Peru, Morocco
Specific gravity7.4–7.6
CleavagePerfect cubic

How to identify Galena

  1. Perfect cubic cleavage
  2. Very heavy (SG ~7.5)
  3. Soft; gray-black streak

Collector notes

  • Often the chief silver ore historically via argentiferous galena
  • Cubic crystals can look like metallic dice

Value context: Ore by Pb/Ag content; sharp cubic crystals are popular teaching specimens.

Galena FAQ

How do you identify Galena?

Galena (PbS) is typically recognized by lead-gray color, metallic luster, Mohs hardness 2.5, and cubic crystal system. RockScan can suggest Galena from a photo and surface these checks on the result card.

What is Galena made of?

Galena composition: Lead sulfide. It forms via hydrothermal veins and mississippi valley-type deposits and is found in USA, Australia, China, Peru, Morocco.

Is Galena valuable?

Ore by Pb/Ag content; sharp cubic crystals are popular teaching specimens.