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How to identify Galena

Lead(II) sulfide (PbS)

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To correctly identify Galena (Lead(II) sulfide (PbS)), check each of these features in order. Many rocks and minerals look alike, so cross-reference multiple properties before deciding.

Step-by-step identification

  1. 1

    Color

    Overall color and any zoning or banding

    Lead-gray, often tarnishing to a dull gray or iridescent blue/purple.

  2. 2

    Luster

    How the surface reflects light: metallic, vitreous, dull

    Bright metallic, becoming dull on tarnished surfaces.

  3. 3

    Texture

    Grain size and surface feel: coarse, fine, glassy

    Typically massive, granular, or in well-formed cubic or cubo-octahedral crystals. Can also be fibrous.

  4. 4

    Crystal Form

    Shape of visible crystals or crystal faces

    Cubic, cubo-octahedral, or octahedral crystals are common. Also massive, granular, or fibrous aggregates.

  5. 5

    Cleavage

    How it breaks: flat cleavage planes vs irregular fracture

    Perfect cubic cleavage in three directions at 90 degrees, producing characteristic step-like fractures or breaking into cubes.

  6. 6

    Geological Environment

    The rock formation and setting where it occurs

    Hydrothermal veins, Mississippi Valley-type (MVT) deposits, contact metamorphic deposits, and less commonly in some igneous rocks.

Key Facts

Hardness
2.5-2.75 on the Mohs scale
Specific Gravity
7.4-7.6 (very high)
Crystal System
Isometric (cubic)
Color
Lead-gray, often tarnishing to dull gray or iridescent
Luster
Metallic
Transparency
Opaque
Fracture
Subconchoidal to uneven, but rarely observed due to perfect cleavage
Cleavage
Perfect cubic {001}
Composition
Lead(II) sulfide (PbS)

Physical characteristics

  • Crystal Habit: Cubic, cubo-octahedral, octahedral, massive, granular, fibrous
  • Cleavage Type: Perfect cubic {001}
  • Fracture Type: Subconchoidal to uneven
  • Tenacity: Brittle
  • Luster Type: Metallic

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