Rock Identifier
Blue glassy mineral fragment, likely kyanite or blue corundum (Tentatively kyanite (Al₂SiO₅); visual identification is uncertain from the photograph) — mineral
mineral

Blue glassy mineral fragment, likely kyanite or blue corundum

Tentatively kyanite (Al₂SiO₅); visual identification is uncertain from the photograph

AI-generated identification · may be incorrect

Bright cobalt-blue, translucent to transparent fragment with vitreous luster and irregular cleavage/fracture. Kyanite hardness is 4.5–5 parallel to length and 6.5–7 across it; corundum would be much harder (Mohs 9).

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Physical properties

Bright cobalt-blue, translucent to transparent fragment with vitreous luster and irregular cleavage/fracture. Kyanite hardness is 4.5–5 parallel to length and 6.5–7 across it; corundum would be much harder (Mohs 9).

Formation & geological history

If kyanite, it formed during regional metamorphism of aluminum-rich sediments, commonly in schist and gneiss, typically during Paleozoic–Precambrian mountain building. The fragment appears natural but may be cut or broken.

Uses & applications

Kyanite is used in refractory ceramics, kiln materials, and occasionally as a gemstone; blue corundum is valued as sapphire. Commercial value depends strongly on confirmed identity, transparency, color, and treatment.

Geological facts

The intense blue color is characteristic of gem-quality kyanite or sapphire, but the visible shape and lack of diagnostic crystal form prevent confident separation from blue glass or treated material.

Field identification & locations

Test hardness, specific gravity, and refractive index; kyanite commonly shows bladed crystals and strong directional hardness, while sapphire scratches glass readily and has much higher density. Common sources include Nepal, India, Kenya, Tanzania, Brazil, and Sri Lanka.