Rock Identifier
Obsidian (likely snowflake or smoky obsidian fragment) (Volcanic glass; predominantly rhyolitic silica glass (SiO₂-rich)) — igneous
igneous

Obsidian (likely snowflake or smoky obsidian fragment)

Volcanic glass; predominantly rhyolitic silica glass (SiO₂-rich)

AI-generated identification · may be incorrect

Typically black to brown, vitreous/glassy luster, conchoidal fracture, no visible crystals or cleavage; Mohs hardness about 5–5.5, specific gravity 2.3–2.6. The specimen appears dark, translucent at edges, and possibly weathered or polished.

Identified More igneous
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Physical properties

Typically black to brown, vitreous/glassy luster, conchoidal fracture, no visible crystals or cleavage; Mohs hardness about 5–5.5, specific gravity 2.3–2.6. The specimen appears dark, translucent at edges, and possibly weathered or polished.

Formation & geological history

Forms when silica-rich lava cools so rapidly that crystals cannot grow, usually in young volcanic flows, domes, and lava margins. Commonly Quaternary to recent, though older obsidian also occurs.

Uses & applications

Used historically for exceptionally sharp blades and arrowheads; today it is collected, carved, polished, and occasionally used in jewelry or ornamental objects.

Geological facts

Fresh fracture edges can be sharper than surgical steel, although obsidian is brittle. Brown or smoky coloration commonly results from iron-bearing impurities or microscopic inclusions.

Field identification & locations

Identify it by glassy luster, sharp curved fracture surfaces, lack of crystal grains, and translucency along thin edges; a steel point may scratch it slightly. Common sources include Mexico, the western United States, Iceland, Armenia, and Japan.