mineral

Quartz (Druzy or Geode fragment)

Silicon Dioxide (SiO2)

AI-generated identification · may be incorrect

Hardness: 7 on Mohs scale; Color: Clear to milky white; Luster: Vitreous (glassy); Crystal Structure: Hexagonal/Trigonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.

Hardness: 7 on Mohs scale
Color: Clear to milky white
Luster: Vitreous (glassy)

Identified March 20, 2026More mineral →

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Physical properties

Hardness: 7 on Mohs scale; Color: Clear to milky white; Luster: Vitreous (glassy); Crystal Structure: Hexagonal/Trigonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.

Formation & geological history

Formed from silica-rich hydrothermal fluids cooling in rock cavities or veins. This specimen appears to be a fragment of a geode or a druzy crust, often found in volcanic or sedimentary host rocks.

Uses & applications

Commonly used in jewelry as semi-precious stones, in electronics for its piezoelectric properties (oscillators), and as a popular specimen for mineral collectors.

Geological facts

Quartz is the second most abundant mineral in Earth's continental crust. It is highly resistant to both chemical and physical weathering, which is why it is the primary component of most river and beach sand.

Field identification & locations

Identify in the field by its inability to be scratched by a steel knife and its lack of cleavage (it breaks into irregular, curved shards). Look for it in gravel pits, mountain outcrops, or inside hollow sedimentary nodules.