Mineral-like Industrial Smelting Waste

Iron Slag (Industrial Byproduct)

Anthropogenic Vitrification Product/Ferrous Slag

Hardness: 5.5-6.5 (Mohs scale); Color: Rusty brown, reddish-orange (due to iron oxidation), with dark grey or glass-like interior; Luster: Sub-metallic to vitreous (glassy); Structure: Vesicular (full of gas bubbles/pockets); Specific Gravity: High (relatively heavy due to iron content).

Hardness: 5
Luster: Sub-metallic to vitreous (glassy)

Identified April 14, 2026More mineral-like industrial smelting waste →

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Physical properties

Formation & geological history

Formed as a byproduct of the iron and steel smelting process where impurities from ore are melted and separated. It cooling rapidly leads to its glass-like or bubbly texture. These are found in areas with historical or current industrial smelting activity.

Uses & applications

Used in construction, road base, asphalt aggregate, and as a raw material in the manufacture of cement and mineral wool insulation.

Geological facts

Slag is often mistaken for meteorites or volcanic rock (like scoria) due to its holes (vesicles) and dark color. However, its glassy texture and specific historical context often point to man-made origins.

Field identification & locations

Identify in the field by looking for 'bubbles' (vesicles) that are perfectly round or have molten flow lines, as well as its discovery near historical railroad tracks, factories, or mines. It is usually non-magnetic or weakly magnetic.

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