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 (Mohs scale); Color: Jet black to dark grey; Luster: Vitreous/Glassy; Structure: Amorphous (non-crystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.35–2.6

Hardness
5–5
Color
Jet black to dark grey
Luster
Vitreous/Glassy
Identified More igneous

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Physical properties

Hardness: 5–5.5 (Mohs scale); Color: Jet black to dark grey; Luster: Vitreous/Glassy; Structure: Amorphous (non-crystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.35–2.6

Formation & geological history

Formed through the rapid cooling of silica-rich (felsic) lava from volcanic eruptions, preventing crystal growth. Most specimens found today are from the Quaternary period (less than 2.6 million years old).

Uses & applications

Used historically for sharp tools and weapons (arrowheads/knives); currently used for jewelry, decorative carvings, scalpel blades in specialized surgery, and metaphysical collecting.

Geological facts

Obsidians are technically 'frozen liquids' rather than true minerals because they lack a crystal structure. Ancient civilizations like the Aztecs and Mayans used polished obsidian as mirrors and currency.

Field identification & locations

Identify by its distinctive shell-like (conchoidal) fracture and sharp edges. Commonly found in volcanic regions such as the American West (Oregon, California), Mexico, Iceland, and Japan.