Rock Identifier
Obsidian (Obsidian (principally SiO2 with MgO and Fe3O4)) — igneous
igneous

Obsidian

Obsidian (principally SiO2 with MgO and Fe3O4)

Hardness: 5–5.5 (Mohs); Color: Black (sometimes brown or sheen depending on inclusions); Luster: Vitreous/Glassy; Structure: Amorphous (non-crystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.35–2.6.

Hardness
5–5
Color
Black (sometimes brown or sheen depending on inclusions)
Luster
Vitreous/Glassy
Identified More igneous

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Physical properties

Hardness: 5–5.5 (Mohs); Color: Black (sometimes brown or sheen depending on inclusions); Luster: Vitreous/Glassy; Structure: Amorphous (non-crystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.35–2.6.

Formation & geological history

Formed when felsic lava extruded from a volcano cools rapidly with minimal crystal growth. It occurs in geologically recent volcanic areas, typically from the Tertiary to Quaternary periods, as it eventually de-vitrifies over millions of years.

Uses & applications

Used historically for sharp tools and weapons (arrowheads, knives); currently used in high-end surgical scalpels, jewelry (beads and cabochons), and as a decorative stone in architecture and landscaping.

Geological facts

Obsidian is technically a 'mineraloid' rather than a mineral because it lacks a crystalline structure. Some varieties like 'Snowflake Obsidian' contain white crystal inclusions called spherulites. It has been traded across continents for over 10,000 years.

Field identification & locations

Identify by its distinct jet-black glossy surface and sharp, curved (conchoidal) edges where broken. Commonly found in volcanic regions like the American Northwest (Oregon), Iceland, Mexico, and Japan. If you hold a thin flake to the light, it is often translucent at the edges.