Rock Identifier
Possible tektite or volcanic glass specimen (Natural silica glass; composition commonly near SiO₂, but exact identification requires chemical testing) — mineral
mineral

Possible tektite or volcanic glass specimen

Natural silica glass; composition commonly near SiO₂, but exact identification requires chemical testing

AI-generated identification · may be incorrect

Black to dark brown, vitreous-to-resinous luster, strongly convoluted or fluted surface, and no visible crystal structure; hardness is typically about 5–6 Mohs. The elongated shape and glossy, flow-like texture may also resemble industrial slag, so visual identification is uncertain.

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Physical properties

Black to dark brown, vitreous-to-resinous luster, strongly convoluted or fluted surface, and no visible crystal structure; hardness is typically about 5–6 Mohs. The elongated shape and glossy, flow-like texture may also resemble industrial slag, so visual identification is uncertain.

Formation & geological history

If genuine, it may be a tektite formed by meteorite-impact melting, or volcanic glass such as obsidian formed by rapid cooling of silica-rich lava; age depends on locality. The pictured surface could alternatively be weathered anthropogenic slag.

Uses & applications

Tektites and obsidian are mainly collector specimens; obsidian is used for ornaments, tools, and occasionally jewelry. Slag has little geological or commercial value.

Geological facts

Tektites commonly show aerodynamic forms and sculpted ablation surfaces, while obsidian usually has conchoidal fracture and a more uniformly glassy texture.

Field identification & locations

Check for conchoidal fracture, low density, bubbles, magnetic response, and a fresh unweathered surface; laboratory XRF, specific gravity, and microscopy are needed to distinguish tektite, obsidian, and slag. Common tektite localities include Southeast Asia, Australia, and North America.