Rock Identifier
Ferrochrome Slag (Industrial Glassy Slag (Fe-Cr alloy byproduct)) — Antropogenic (Man-made industrial byproduct)
Antropogenic (Man-made industrial byproduct)

Ferrochrome Slag

Industrial Glassy Slag (Fe-Cr alloy byproduct)

Hardness: 6-7 (Mohs); Color: Dark grey to greenish-black with metallic flecks; Luster: Vitreous (glassy) to metallic; Crystal Structure: Amorphous/microcrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 3.0-4.0

Hardness
6-7 (Mohs)
Color
Dark grey to greenish-black with metallic flecks
Luster
Vitreous (glassy) to metallic

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Physical properties

Hardness: 6-7 (Mohs); Color: Dark grey to greenish-black with metallic flecks; Luster: Vitreous (glassy) to metallic; Crystal Structure: Amorphous/microcrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 3.0-4.0

Formation & geological history

Formed as a byproduct of the smelting process in the production of ferrochromium. Molten waste is cooled rapidly, resulting in a dense, glassy material. Often found in areas with a history of steel or alloy manufacturing.

Uses & applications

Commonly used as construction aggregate, road base material, or abrasive grit for sandblasting. Some pieces are collected as 'curiosity' stones or 'meteor-wrongs' due to their metallic appearance.

Geological facts

Slag is frequently mistaken for meteorites because of its high density, dark color, and occasional magnetism. It often contains vesicles (small bubble holes) from trapped gases during cooling, which the specimen in the image appears to exhibit.

Field identification & locations

Identify by looking for air bubbles (vesicles), a glassy 'conchoidal' fracture, and unusual heaviness. It is commonly found near old railways, industrial sites, or used as gravel in rural roads. Collectors should test for magnetism and look for lack of a 'fusion crust' to distinguish from real meteorites.