Rock Identifier
Quartz geode or drusy quartz cluster (Quartz (silicon dioxide, SiO₂), likely a quartz-lined cavity in host rock) — mineral
mineral

Quartz geode or drusy quartz cluster

Quartz (silicon dioxide, SiO₂), likely a quartz-lined cavity in host rock

AI-generated identification · may be incorrect

Typically hardness 7 Mohs, white to colorless, vitreous to sparkling drusy luster, and trigonal crystal structure with no cleavage. The granular cavity lining and translucent crystals are characteristic of quartz, though the specimen may include carbonate or other host minerals.

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Physical properties

Typically hardness 7 Mohs, white to colorless, vitreous to sparkling drusy luster, and trigonal crystal structure with no cleavage. The granular cavity lining and translucent crystals are characteristic of quartz, though the specimen may include carbonate or other host minerals.

Formation & geological history

Forms when silica-rich groundwater fills cavities in volcanic rock, sediment, or hydrothermal veins; quartz crystals grow inward over long periods, commonly from the Cenozoic to older geologic ages. The exact age and host rock cannot be determined from the image.

Uses & applications

Used as a decorative specimen, lapidary material, and source of collectible crystal clusters; quartz is also important in glass, electronics, abrasives, and engineered stone. This piece is primarily a display specimen.

Geological facts

The sparkling surface is drusy quartz—many tiny crystals coating a cavity. Quartz is abundant worldwide and is piezoelectric, producing an electrical charge when mechanically stressed.

Field identification & locations

Identify by its glassy sparkle, hardness, lack of cleavage, and inability to be scratched by a steel knife; it should scratch glass. Common sources include Brazil, Uruguay, Morocco, Mexico, and the United States.