Rock Identifier
Quartz (likely druzy quartz) (Quartz, silicon dioxide (SiO₂)) — mineral
mineral

Quartz (likely druzy quartz)

Quartz, silicon dioxide (SiO₂)

AI-generated identification · may be incorrect

White to translucent, glassy luster with a sugary coating of tiny crystals; Mohs hardness 7, no cleavage, conchoidal fracture, and a hexagonal crystal structure. The cream-colored outer material may include iron-stained quartz or a carbonate matrix.

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Physical properties

White to translucent, glassy luster with a sugary coating of tiny crystals; Mohs hardness 7, no cleavage, conchoidal fracture, and a hexagonal crystal structure. The cream-colored outer material may include iron-stained quartz or a carbonate matrix.

Formation & geological history

Likely formed when silica-rich hydrothermal fluids deposited quartz in a cavity or on a host rock; the specimen appears natural but may be broken from a larger formation. Exact geological age and locality cannot be determined from the image.

Uses & applications

Common quartz is used in glass, ceramics, abrasives, electronics, and countertops; attractive druzy specimens are sold for mineral collecting and occasionally jewelry.

Geological facts

Druzy quartz consists of many microscopic quartz crystals coating a surface, producing a sparkly sugar-like texture. Quartz is one of Earth’s most abundant and chemically durable minerals.

Field identification & locations

Identify it by its hardness, glassy sparkle, lack of cleavage, and inability to scratch it with a steel knife while it can scratch ordinary glass. Common worldwide, especially in hydrothermal veins and geodes.