Rock Identifier
Mahogany Obsidian (Obsidian (Volcanic Glass with Hematite/Magnetite inclusions), SiO2) — igneous
igneous

Mahogany Obsidian

Obsidian (Volcanic Glass with Hematite/Magnetite inclusions), SiO2

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: 2.35-2.6

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: 2.35-2.6

Formation & geological history

Formed from rapidly cooling extrusive igneous lava, specifically rhyolitic lava. The mahogany color comes from the inclusion of iron oxides (Hematite or Magnetite) during the cooling process. Common in Pliocene to Holocene volcanic fields.

Uses & applications

Used primarily in jewelry-making for cabochons and beads, as a lapidary material for decorative carvings, and in metaphysical practices. Historically used to craft sharp blades and arrowheads.

Geological facts

Despite looking like a mineral, it is actually a 'mineraloid' because it lacks a crystalline structure. The reddish-brown 'mahogany' swirls are essentially rusted iron trapped within the volcanic glass.

Field identification & locations

Identify by its glass-like texture, sharp conchoidal edges when broken, and distinctive brick-red patterns against a black base. Commonly found in North America (USA-Oregon, Mexico), Japan, and Afghanistan.