
Mineral-like byproduct
Iron Slag
Anthropogenic Vitreous Silicate (Byproduct of Smelting)
Hardness: 5-6 (Mohs); Color: Dark grey, black, or metallic; Luster: Sub-metallic to glassy; Structure: Amorphous/vesicular; Cleavage: None; Specific Gravity: 2.8 - 4.5.
- Hardness
- 5-6 (Mohs)
- Color
- Dark grey, black, or metallic
- Luster
- Sub-metallic to glassy
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Physical properties
Hardness: 5-6 (Mohs); Color: Dark grey, black, or metallic; Luster: Sub-metallic to glassy; Structure: Amorphous/vesicular; Cleavage: None; Specific Gravity: 2.8 - 4.5.
Formation & geological history
Formed during the industrial smelting process where impurities (like silica and alumina) are separated from molten metal ore. It is an artificial rock rather than a natural geological formation.
Uses & applications
Historically used for road ballast, concrete aggregate, and track bedding. Occasionally used in rustic landscaping or as a historical artifact in archaeological contexts.
Geological facts
Slag is often mistaken for meteorites due to its dark, melted appearance and occasional magnetic properties, but its internal bubbles (vesicles) are a clear indicator of industrial origin.
Field identification & locations
Identify in the field by looking for gas bubbles, flow textures, or a glassy fracture on broken edges. Commonly found near old railroad tracks, industrial sites, and historical foundry ruins.
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