Rock Identifier
Cullet Glass (Industrial Slag Glass) (Amorphous Silica (SiO2) with metallic oxide impurities) — Man-made byproduct (often mistaken for Obsidian or Emerald)
Man-made byproduct (often mistaken for Obsidian or Emerald)

Cullet Glass (Industrial Slag Glass)

Amorphous Silica (SiO2) with metallic oxide impurities

Hardness: 5.5-6.5 on Mohs scale; Color: Deep forest green; Luster: Vitreous (glassy); Structure: Amorphous (non-crystalline); Cleavage: None (conchoidal fracture); Presence of small internal gas bubbles.

Hardness
5
Color
Deep forest green
Luster
Vitreous (glassy)

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Physical properties

Hardness: 5.5-6.5 on Mohs scale; Color: Deep forest green; Luster: Vitreous (glassy); Structure: Amorphous (non-crystalline); Cleavage: None (conchoidal fracture); Presence of small internal gas bubbles.

Formation & geological history

Formed as a waste product from glass manufacturing or smelting processes. Molten glass leftovers are dumped and cooled rapidly, creating a glassy, non-crystalline solid. Unlike natural obsidian, it is anthropomorphic in origin.

Uses & applications

Commonly used in landscaping, aquarium decor, or as a source material for decorative glass 'gemstones'. Occasionally used in wire-wrapped jewelry as a simulated forest green obsidian or aventurine.

Geological facts

Green cullet glass is often found near historic glass factory sites. Because it exhibits the same curved (conchoidal) fractures as obsidian, it is frequently misidentified as volcanic glass or rough emerald by novice collectors.

Field identification & locations

Identify in the field by looking for spherical gas bubbles (not found in natural gems), a very uniform color, and a lack of flow banding or mineral inclusions. Often found in riverbeds near old industrial towns or construction fill.