Rock Identifier
Obsidian (in jewelry setting) (Volcanic Glass (Amorphous Silica)) — igneous
igneous

Obsidian (in jewelry setting)

Volcanic Glass (Amorphous Silica)

Hardness: 5-5.5 (Mohs scale); Color: Typically deep black (due to iron and magnesium); Luster: Vitreous/Glassy; Structure: Amorphous (non-crystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.3 - 2.6.

Hardness
5-5
Color
Typically deep black (due to iron and magnesium)
Luster
Vitreous/Glassy
Identified More igneous

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Physical properties

Hardness: 5-5.5 (Mohs scale); Color: Typically deep black (due to iron and magnesium); Luster: Vitreous/Glassy; Structure: Amorphous (non-crystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.3 - 2.6.

Formation & geological history

Formed through the rapid cooling of felsic lava, which prevents the growth of mineral crystals. It is common in volcanically active regions and is generally geologically young (less than 65 million years) as glass eventually devitrifies.

Uses & applications

Used primarily for jewelry, ornamental objects, and surgical scalpel blades (due to its ability to be honed to an edge much sharper than steel). It is also highly valued by gemstone collectors and for decorative metaphysical items.

Geological facts

Because it breaks with a conchoidal fracture, it creates edges that are molecularly thin. In the Stone Age, it was the primary material for high-quality arrowheads and blades. It shares the same chemical composition as granite but cooled too fast to crystallize.

Field identification & locations

Identify in the field by its characteristic glassy texture and curved, shell-like (conchoidal) fractures. Found in volcanic areas with silica-rich lava such as the Western USA, Mexico, Iceland, and Japan. Collectors look for unique variations like 'snowflake' or 'rainbow' obsidian.