Anthropogenic Material (Man-made Rock)
Ferrous Slag (Iron Smelting By-product)
Fused Siliceous Slag
Hardness: 6-7 (Mohs); Color: Olive green to dark brownish-black; Luster: Vitreous to dull; Structure: Non-crystalline/Amorphous; Cleavage: Conchoidal fracture; Features: Vesicles (gas bubbles), flow lines, and glassy texture.
- Hardness
- 6-7 (Mohs)
- Color
- Olive green to dark brownish-black
- Luster
- Vitreous to dull
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Physical properties
Hardness: 6-7 (Mohs); Color: Olive green to dark brownish-black; Luster: Vitreous to dull; Structure: Non-crystalline/Amorphous; Cleavage: Conchoidal fracture; Features: Vesicles (gas bubbles), flow lines, and glassy texture.
Formation & geological history
Formed as a byproduct of the iron smelting process. During smelting, impurities (gangue) are removed from iron ore and fused with flux (like limestone) at high temperatures to form a liquid melt that cools into this rock-like substance.
Uses & applications
Used historically and currently for road aggregate, railroad ballast, concrete manufacturing, and as abrasive grit. Some colorful pieces are used in lapidary work as 'Leland Blue' or 'Sieber Agate'.
Geological facts
Slag can often be mistaken for volcanic rock (basalt or obsidian) or meteorites due to its weight and vesicles. It is actually one of the most common 'fake' rock finds in industrial regions.
Field identification & locations
Look for the presence of vesicles (bubbles) and a glassy, conchoidal fracture. In the field, look for proximity to old railroad beds, iron works, or historic industrial sites. It is often non-magnetic or weakly magnetic compared to iron ore.
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