Rock Identifier
Rainbow Obsidian (Volcanic glass (SiO2 - approximately 70% or more silicon dioxide)) — Igneous
Igneous

Rainbow Obsidian

Volcanic glass (SiO2 - approximately 70% or more silicon dioxide)

Hardness: 5-5.5 (Mohs scale); Color: Black with colorful iridescence (purple, green, gold); Luster: Vitreous/Glassy; Structure: Amorphous (non-crystalline); Cleavage: Conchoidal fracture; Specific gravity: 2.4

Hardness
5-5
Color
Black with colorful iridescence (purple, green, gold)
Luster
Vitreous/Glassy
Identified More igneous

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Physical properties

Hardness: 5-5.5 (Mohs scale); Color: Black with colorful iridescence (purple, green, gold); Luster: Vitreous/Glassy; Structure: Amorphous (non-crystalline); Cleavage: Conchoidal fracture; Specific gravity: 2.4

Formation & geological history

Formed from the rapid cooling of silica-rich (felsic) lava, which prevents crystal growth. The 'rainbow' effect is caused by microscopic inclusions of magnetite or nanobubbles of gas trapped during flow. Geological age varies by site, typically Cenozoic Era.

Uses & applications

Used primarily in jewelry (beads, cabochons), ornamental carvings, and for spiritual/metaphysical collecting. Historically used for extremely sharp cutting tools and scalpels.

Geological facts

The rainbow sheen is actually an optical phenomenon caused by light diffraction on layers of mineral inclusions rather than pigment. It is one of the sharpest naturally occurring materials; its edges can be thinner than a molecule of steel.

Field identification & locations

Identify in the field by its glassy texture and conchoidal 'shell-like' fractures. While it looks solid black in shade, the rainbow sheen is revealed under direct, bright light. Common locations include Mexico (Jalisco), Northern California (Glass Mountain), and Oregon.