Rock Identifier
Obsidian (Obsidian (principally SiO2/Silicon dioxide)) — igneous
igneous

Obsidian

Obsidian (principally SiO2/Silicon dioxide)

Hardness: 5-6 (Mohs); Color: Jet black to dark brownish-red; Luster: Vitreous/Glassy; Structure: Amorphous (non-crystalline); Fracture: Conchoidal (shell-like curves); Specific Gravity: 2.3 - 2.6.

Hardness
5-6 (Mohs)
Color
Jet black to dark brownish-red
Luster
Vitreous/Glassy
Identified More igneous

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Physical properties

Hardness: 5-6 (Mohs); Color: Jet black to dark brownish-red; Luster: Vitreous/Glassy; Structure: Amorphous (non-crystalline); Fracture: Conchoidal (shell-like curves); Specific Gravity: 2.3 - 2.6.

Formation & geological history

Formed through the rapid cooling of silica-rich felsic lava, preventing crystal growth. Most specimens date from the Pliocene to the Holocene, as obsidian is geologically unstable and eventually devitrifies into minerals like quartz over millions of years.

Uses & applications

Used historically for razor-sharp tools and weapons. Currently used in jewelry (bracelets, beads), decorative carvings, and in high-precision surgical scalpel blades because it holds an edge sharper than steel.

Geological facts

Obsidian fractures down to a single atom, making its edge much sharper than a surgical steel scalpel. Native Americans used it for arrowheads and trade, with some pieces traveling thousands of miles from their source.

Field identification & locations

Identify in the field by its characteristic conchoidal fracture which leaves sharp, curved edges. Look for it in volcanic regions such as the American Northwest (Oregon/California) or Iceland. Always check for translucent edges when held to a light source.