
not a natural rock
Man-made Slag (Industrial Byproduct)
Anthropogenic Glassy Residue
Hardness: 5.5-6.5 (Mohs scale); Color: Black, dark gray, or multi-colored; Luster: Vitreous to dull; Structure: Amorphous/Glassy; Cleavage: Conchoidal fracture; Specific Gravity: 2.5-4.0 (highly variable)
- Hardness
- 5
- Color
- Black, dark gray, or multi-colored
- Luster
- Vitreous to dull
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Physical properties
Hardness: 5.5-6.5 (Mohs scale); Color: Black, dark gray, or multi-colored; Luster: Vitreous to dull; Structure: Amorphous/Glassy; Cleavage: Conchoidal fracture; Specific Gravity: 2.5-4.0 (highly variable)
Formation & geological history
Formed as a byproduct of smelting ores (iron, steel, copper) where impurities are separated from molten metal. This specimen appears to be modern industrial waste rather than a natural geological formation.
Uses & applications
Used in construction as road base, railroad ballast, or aggregate in concrete. Occasionally used in the production of mineral wool insulation.
Geological facts
Slag can often be mistaken for obsidian or meteorites, but the presence of vesicles (gas bubbles) or bits of embedded metal often distinguishes it as industrial in origin.
Field identification & locations
Commonly found near historical smelting sites, railroads, or landfills. Identified by its weight, glassy texture, and lack of natural crystalline structure typical of minerals.
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