Rock Identifier
Obsidian (Volcanic Glass (SiO2, usually >70% silica content)) — Igneous
Igneous

Obsidian

Volcanic Glass (SiO2, usually >70% silica content)

Hardness: 5-5.5 on Mohs scale; Color: typically jet black but can be brown, gray, or green; Luster: Vitreous (glassy); Structure: Amorphous (non-crystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.4

Hardness
5-5
Color
typically jet black but can be brown, gray, or green
Luster
Vitreous (glassy)
Identified More igneous

Identify your own rocks.

Get a report just like this from any photo, free.

Physical properties

Hardness: 5-5.5 on Mohs scale; Color: typically jet black but can be brown, gray, or green; Luster: Vitreous (glassy); Structure: Amorphous (non-crystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.4

Formation & geological history

Formed through the rapid cooling of silicious lava, which prevents the growth of crystals. It is typically found in geologically recent volcanic areas (Cenozoic era) because it is metastable and eventually devitrifies into fine-grained crystals over millions of years.

Uses & applications

Historically used for making sharp weapons and cutting tools; currently used in modern surgery for high-precision scalpels, ornamental jewelry (beads, cabochons), and as a gemstone for collectors.

Geological facts

Because it has no crystal structure, obsidian fractures with extremely sharp edges—sometimes down to molecular thinness. Native Americans and other ancient civilizations used it to create arrowheads, spear points, and mirrors.

Field identification & locations

Identify in the field by its intense glassy sheen and characteristic curved 'clamshell-like' (conchoidal) fractures. Primarily found in volcanic regions of the Western USA (Oregon, California), Mexico, Iceland, and Italy (Lipari). Note: it is easily scratched by steel compared to quartz.