Rock Identifier
Green Slag Glass (Amorphous Silica Glass (Anthropogenic)) — Industrial byproduct (often mistaken for obsidian or mineral)
Industrial byproduct (often mistaken for obsidian or mineral)

Green Slag Glass

Amorphous Silica Glass (Anthropogenic)

Hardness: 5.5-6 on Mohs scale. Color: Teal to sea-green, often with white or grey crusting. Luster: Vitreous (glassy) when broken, dull when weathered. Structure: Amorphous (non-crystalline). Cleavage: None, exhibits conchoidal fracture. Often contains spherical gas bubbles (vesicles).

Hardness
5
Color
Teal to sea-green, often with white or grey crusting
Luster
Vitreous (glassy) when broken, dull when weathered

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Physical properties

Hardness: 5.5-6 on Mohs scale. Color: Teal to sea-green, often with white or grey crusting. Luster: Vitreous (glassy) when broken, dull when weathered. Structure: Amorphous (non-crystalline). Cleavage: None, exhibits conchoidal fracture. Often contains spherical gas bubbles (vesicles).

Formation & geological history

Formed as a byproduct of smelting iron, copper, or other ores in blast furnaces. Impurities like limestone, silica, and mineral oxides are removed from metal and cool into glass. Most specimens found in the US date to the 19th or early 20th centuries.

Uses & applications

Historically used as railroad ballast, road fill, or discarded as waste. Currently popular among rockhounds and lapidaries for tumble polishing, aquarium decor, and folk art jewelry.

Geological facts

Also known as 'Leland Blue' or 'Frankfurt Green' depending on the region and the specific smelter it came from. Its color is often caused by trace amounts of chemical additives like copper or chromium used in the industrial process.

Field identification & locations

Identify by looking for spherical bubbles (which do not occur in natural obsidian) and conchoidal fractures. Commonly found near historical iron working sites, old railway beds, and Great Lakes beaches. It is a sign of local industrial history.