Rock Identifier
Iron Slag (Anthropogenic Vitreous Silicate (Byproduct of Smelting)) — Mineral-like byproduct
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
Identified More mineral-like byproduct

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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.