Rock Identifier
Obsidian (Volcanic Glass (SiO2 rich)) — igneous
igneous

Obsidian

Volcanic Glass (SiO2 rich)

Hardness: 5-5.5 | Color: Typically black, but can be brownish or reddish | Luster: Vitreous (glassy) | Crystal Structure: Amorphous (non-crystalline) | Cleavage: None (conchoidal fracture) | Specific Gravity: 2.35-2.6

Hardness
5-5
Identified More igneous

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Physical properties

Hardness: 5-5.5 | Color: Typically black, but can be brownish or reddish | Luster: Vitreous (glassy) | Crystal Structure: Amorphous (non-crystalline) | Cleavage: None (conchoidal fracture) | Specific Gravity: 2.35-2.6

Formation & geological history

Obsidian forms when silica-rich felsic lava cools extremely rapidly, which prevents the growth of crystals. It is typically found in volcanic regions of various ages, though it can devitrify over millions of years into more stable minerals.

Uses & applications

Historically used for surgical blades and knapping into sharp tools/weapons (arrows, spears); currently used in jewelry (beads, cabochons), modern scalpels for precision surgery, and as a popular collector's stone.

Geological facts

Because it's a glass, it breaks with sharp edges like a razor, down to a single molecule thick. In many cultures, like the Aztecs and Mayans, it was a vital trade commodity for making ceremonial knives and mirrors.

Field identification & locations

Identify in the field by its distinct conchoidal (shell-like) fracture pattern and extremely glossy, smooth surface. It is commonly found in the Pacific Northwest (USA), Mexico, Iceland, and Japan. Collectors should look for unique variations like 'Snowflake' or 'Rainbow' obsidian.