Rock Identifier
Polished mahogany obsidian (probable) (Volcanic glass; primarily rhyolitic silica glass (SiO₂), with iron-oxide inclusions) — igneous
igneous

Polished mahogany obsidian (probable)

Volcanic glass; primarily rhyolitic silica glass (SiO₂), with iron-oxide inclusions

AI-generated identification · may be incorrect

Hardness about 5–5.5 Mohs; dark brown to black with mahogany-red and possibly golden patches, vitreous luster, conchoidal fracture, and no cleavage. The rounded shape indicates tumbling or polishing.

Identified More igneous
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Physical properties

Hardness about 5–5.5 Mohs; dark brown to black with mahogany-red and possibly golden patches, vitreous luster, conchoidal fracture, and no cleavage. The rounded shape indicates tumbling or polishing.

Formation & geological history

Formed when silica-rich lava cooled too rapidly for crystals to grow, producing natural volcanic glass; red-brown areas generally reflect dispersed iron oxides. Most examples are Quaternary to late Cenozoic and commonly originate in volcanic regions of the western United States.

Uses & applications

Used for cabochons, beads, carvings, ornaments, and collectors’ specimens; historically, obsidian was knapped into sharp tools and projectile points.

Geological facts

Mahogany obsidian is a color variety rather than a separate mineral species. Its glassy fracture can produce edges sharper than surgical steel, though this polished piece is not sharp.

Field identification & locations

Identify by its glassy appearance, rounded conchoidal surfaces, lack of visible crystals, and brown-red swirls or patches; distinguish it from jasper by the absence of granular texture. Common sources include Oregon, California, Utah, Mexico, and Armenia.