Rock Identifier
Mahogany Obsidian (Obsidian (Volcanic Glass) with Hematite/Magnetite inclusions) — igneous
igneous

Mahogany Obsidian

Obsidian (Volcanic Glass) with Hematite/Magnetite inclusions

Hardness: 5-5.5 (Mohs); Color: Dark brown or reddish-brown with black spots; Luster: Vitreous/Glassy; Structure: Amorphous (non-crystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.35-2.6

Hardness
5-5
Color
Dark brown or reddish-brown with black spots
Luster
Vitreous/Glassy
Identified More igneous

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Physical properties

Hardness: 5-5.5 (Mohs); Color: Dark brown or reddish-brown with black spots; Luster: Vitreous/Glassy; Structure: Amorphous (non-crystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.35-2.6

Formation & geological history

Formed through the extremely rapid cooling of felsic lava, preventing crystal growth. Its reddish-brown color is caused by the inclusion of iron-rich minerals like hematite or magnetite during the cooling process. Usually found in geologically recent volcanic areas (Cenozoic era).

Uses & applications

Commonly used in jewelry, lapidary arts (cabochons and beads), and decorative carvings. Historically, obsidian was used for sharp cutting tools and surgical blades; currently popular in the metaphysical and gemstone collecting markets.

Geological facts

Obsidian is often called 'volcanic glass.' While it looks like a mineral, it is technically an 'extrusive igneous rock' because it lacks a crystalline structure. The 'Mahogany' variety is prized for its wavy, wood-grain-like patterns.

Field identification & locations

Identify by its glass-like texture, conchoidal (shell-like) fracture patterns, and its distinct red-and-black mottling. Commonly found in volcanic regions of the Western United States (Oregon, California), Mexico, and Japan.