
mineral
Blue slag glass / industrial glass fragment
Artificial silicate glass, composition variable; likely copper- or cobalt-colored furnace slag
AI-generated identification · may be incorrectVivid translucent blue, glassy luster, conchoidal fracture, and irregular vesicles; no true crystal structure or cleavage. Mohs hardness is approximately 5–6, with moderate-to-high density depending on metal content.…
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Physical properties
Vivid translucent blue, glassy luster, conchoidal fracture, and irregular vesicles; no true crystal structure or cleavage. Mohs hardness is approximately 5–6, with moderate-to-high density depending on metal content. The sharp, melted-looking edges and bubbly texture indicate processed glassy material rather than a natural mineral.
Formation & geological history
Formed when molten industrial waste or glass cooled rapidly, trapping bubbles and producing a quenched amorphous texture; it has no geological age. Exact identification requires chemical testing, such as XRF, because similar blue glass can contain cobalt, copper, or synthetic pigments.
Uses & applications
Primarily a curiosity, decorative specimen, or craft material; it is not generally used as a gemstone or construction stone. Avoid handling sharp edges and do not use it for jewelry without cutting and polishing.
Geological facts
The intense blue color and frothy surface are characteristic of colored glass or slag, not typical natural blue rocks. Natural alternatives such as azurite or sodalite usually show crystalline grains, cleavage, or earthy surfaces.
Field identification & locations
Inspect for conchoidal fracture, bubbles, flow bands, and a uniformly glassy interior; these distinguish it from crystalline rock. Commonly found near historic glassworks, metal-smelting sites, dumps, or beaches receiving industrial debris.
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