
mineral
Galena
Lead Sulfide (PbS)
AI-generated identification · may be incorrectHardness: 2.5 on Mohs scale; Color: Lead-gray to silver-blue; Luster: Metallic; Crystal Structure: Isometric (cubic); Cleavage: Perfect cubic in three directions; Specific Gravity: Very high (7.4 to 7.6).
- Hardness
- 2
- Color
- Lead-gray to silver-blue
- Luster
- Metallic
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Physical properties
Hardness: 2.5 on Mohs scale; Color: Lead-gray to silver-blue; Luster: Metallic; Crystal Structure: Isometric (cubic); Cleavage: Perfect cubic in three directions; Specific Gravity: Very high (7.4 to 7.6).
Formation & geological history
Formed primarily in hydrothermal veins and sedimentary environments through the cooling of mineral-rich fluids or precipitation. It is found in rocks of various geological ages, often associated with sphalerite, pyrite, and quartz.
Uses & applications
Primary ore of lead; used in battery manufacturing, lead-acid batteries, radiation shielding, and ammunition. Historically used for making kohl and silver refining.
Geological facts
Galena is the most important ore of lead and often contains enough silver to be an important silver ore as well. It was used as a semiconductor in early crystal radio sets.
Field identification & locations
Identifiable by its distinct cubic cleavage, high density (unexpectedly heavy for its size), and metallic silver-gray streak. Common locations include Missouri and Kansas (USA), England, and Germany.
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