
mineral
Galena
Lead Sulfide (PbS)
AI-generated identification · may be incorrectHardness: 2.5 on Mohs scale; Color: Lead gray to silver; Luster: Bright metallic (can tarnish); Crystal structure: Isometric (cubic); Specific gravity: High (7.2-7.6); Cleavage: Perfect cubic.
- Hardness
- 2
- Color
- Lead gray to silver
- Luster
- Bright metallic (can tarnish)
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Physical properties
Hardness: 2.5 on Mohs scale; Color: Lead gray to silver; Luster: Bright metallic (can tarnish); Crystal structure: Isometric (cubic); Specific gravity: High (7.2-7.6); Cleavage: Perfect cubic.
Formation & geological history
Hydrothermal mineral found in veins, also in sedimentary rocks as replacements. It is the primary ore of lead and often contains silver.
Uses & applications
Primary source of lead for batteries, ammunition, and radiation shielding; historical source of silver; popular for mineral collectors.
Geological facts
Galena is one of the most abundant and widely distributed sulfide minerals. It often contains up to 1 percent silver as an impurity. Historically, it was used as a semiconductor in early crystal radio sets.
Field identification & locations
Identify by its bright metallic luster, distinctive gray streak, and surprising weight (high density). It feels much heavier than it looks. Common in Missouri, USA (State Mineral), and areas of the UK.
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Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
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Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
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Granite
Granite (Phaneritic intrusive igneous rock)
igneous
Septarian Pebble
Septarian nodule / Concretion
sedimentary