
mineral
Silicon (Industrial Grade)
Elemental Silicon (Si)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Silvery-grey with a blue metallic sheen; Luster: Metallic; Crystal structure: Diamond cubic; Specific Gravity: 2.33 (relatively light for a metallic-looking substance).
- Hardness
- 7 on Mohs scale
- Color
- Silvery-grey with a blue metallic sheen
- Luster
- Metallic
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Physical properties
Hardness: 7 on Mohs scale; Color: Silvery-grey with a blue metallic sheen; Luster: Metallic; Crystal structure: Diamond cubic; Specific Gravity: 2.33 (relatively light for a metallic-looking substance).
Formation & geological history
Produced by the reduction of high-purity silica (quartz) with carbon in electric arc furnaces at temperatures over 1900°C. While silicon is the second most abundant element in Earth's crust, it does not occur naturally in its elemental form.
Uses & applications
Primarily used in the production of aluminum alloys as a strengthening agent, in the chemical industry for silicones, and (when further refined) in solar cells and semiconductors for electronics.
Geological facts
The specimen's light weight (low density) and lack of streak (high hardness) distinguish it from native metals or heavy ores like galena. It is often mistaken for a natural mineral or meteorite by collectors.
Field identification & locations
Identify by its unusually light weight given its metallic appearance, high hardness (it will scratch glass), and brittle, conchoidal fracture pattern. Common in rocky fill or near industrial sites.
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