Rock Identifier
Obsidian (Obsidian (volcanic glass, amorphous silica rich rock)) — Igneous
Igneous

Obsidian

Obsidian (volcanic glass, amorphous silica rich rock)

Hardness: 5-6 on Mohs scale. Color: Typically black, but can be dark brown, green, or rarely blue, red, or iridescent. Luster: Vitreous (glassy). Crystal Structure: Amorphous (no crystal structure). Cleavage: None (conchoidal fracture). Specific Gravity: 2.3-2.6.

Hardness
5-6 on Mohs scale
Luster
Vitreous (glassy)
Identified More igneous

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Physical properties

Hardness: 5-6 on Mohs scale. Color: Typically black, but can be dark brown, green, or rarely blue, red, or iridescent. Luster: Vitreous (glassy). Crystal Structure: Amorphous (no crystal structure). Cleavage: None (conchoidal fracture). Specific Gravity: 2.3-2.6.

Formation & geological history

Formation Process: Rapid cooling of viscous lava, typically felsic (rhyolitic) in composition, which prevents crystal growth. Geological Age: Can be found in areas of recent volcanic activity, ranging from a few thousand years to many millions of years old. Environments: Associated with volcanic eruptions settings where lava flows solidify quickly.

Uses & applications

Industry: Used as a precise cutting edge in surgical scalpels (flaked obsidian) due to its extremely sharp edges. Construction: Historically used in some cultures for building materials. Jewelry: Frequently used as a gemstone, particularly polished and carved into various forms. Collecting Value: Valued by collectors for its unique appearance and origins.

Geological facts

Obsidian is essentially natural glass. Its sharp edges made it highly prized by ancient cultures for tools and weapons, such as arrowheads, spear points, and knives. The extreme sharpness of obsidian blades can exceed that of surgical steel. Rainbow obsidian exhibits an iridescence due to microscopic inclusions of magnetite nanoparticles.

Field identification & locations

How to Identify in the Field: Look for its distinct glassy texture, dark color, and sharp, conchoidal fractures (resembling broken glass). It often occurs in flow bands or layers within volcanic rock formations. Common Locations: Found in volcanically active regions worldwide, including the western United States (e.g., Yellowstone, Oregon), Mexico, Ecuador, Japan, and parts of the Mediterranean. Tips for Collectors: Be aware of its sharpness; handle with care. Look for areas with past or present volcanic activity.