How to identify Galena
Lead(II) sulfide (PbS)
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Open the appTo 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
Color
Overall color and any zoning or banding
Lead-gray, often tarnishing to a dull gray or iridescent blue/purple.
- 2
Luster
How the surface reflects light: metallic, vitreous, dull
Bright metallic, becoming dull on tarnished surfaces.
- 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
Crystal Form
Shape of visible crystals or crystal faces
Cubic, cubo-octahedral, or octahedral crystals are common. Also massive, granular, or fibrous aggregates.
- 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
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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