Rock Identifier
Mahogany Obsidian (Volcanic Glass (SiO2 + Fe2O3)) — igneous
igneous

Mahogany Obsidian

Volcanic Glass (SiO2 + Fe2O3)

Hardness: 5-5.5 (Mohs scale); Color: Black with reddish-brown streaks or mottling; Luster: Vitreous/Glassy; Structure: Amorphous (non-crystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.35-2.60

Hardness
5-5
Color
Black with reddish-brown streaks or mottling
Luster
Vitreous/Glassy
Identified More igneous

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Physical properties

Hardness: 5-5.5 (Mohs scale); Color: Black with reddish-brown streaks or mottling; Luster: Vitreous/Glassy; Structure: Amorphous (non-crystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.35-2.60

Formation & geological history

Formed from the rapid cooling of silica-rich (rhyolitic) lava. Rapid cooling prevents crystal growth. The mahogany color comes from inclusions of Hematite or Magnetite (iron oxides) that were trapped as the lava solidified.

Uses & applications

Used primarily for jewelry (cabochons and beads), ornamental carvings, and metaphysical collecting. Historically used for making sharp-edged tools like arrowheads and knives.

Geological facts

Because it is a glass and not a mineral, it is technically a 'mineraloid'. It has been used since prehistoric times for its ability to produce an edge significantly sharper than even the highest quality steel scalpels.

Field identification & locations

Identify in the field by its distinct conchoidal (shell-like) fracture edges and smooth, glassy surface. Commonly found in volcanic regions of the United States (Oregon, California, Utah), Mexico, and Japan. Collectors should look for high contrast between the red and black patterns.