Rock Identifier
Black Obsidian (Obsidian (Volcanic Glass), primarily SiO2 (Silicon Dioxide) with impurities) — igneous
igneous

Black Obsidian

Obsidian (Volcanic Glass), primarily SiO2 (Silicon Dioxide) with impurities

Hardness: 5–5.5 on Mohs scale; Color: Jet black to dark gray; Luster: Vitreous (glass-like); Crystal Structure: Amorphous (non-crystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.4

Hardness
5–5
Color
Jet black to dark gray
Luster
Vitreous (glass-like)
Identified More igneous

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Physical properties

Hardness: 5–5.5 on Mohs scale; Color: Jet black to dark gray; Luster: Vitreous (glass-like); Crystal Structure: Amorphous (non-crystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.4

Formation & geological history

Formed through the rapid cooling of felsic lava, preventing crystal growth. Most specimens found today are relatively young geologically (Cenozoic to Holocene) as the glass eventually devitrifies into quartz and feldspar over millions of years.

Uses & applications

Used for making jewelry, scalpels for precision surgery due to its molecularly sharp edges, ornamental carvings, and 'scrying' stones in metaphysical communities.

Geological facts

Because it lacks a crystal structure, obsidian edges can reach near-molecular thinness, making it sharper than high-quality steel scalpels. It was used by ancient civilizations for weaponry, such as the Aztec Macuahuitl.

Field identification & locations

Identify by its smooth, glassy surface and characteristic curved (conchoidal) fractures that resemble ripples in water. Commonly found in volcanic regions such as the American Northwest, Mexico, Iceland, and Italy.