
mineral
Quartz Druzy on Geode Fragment
Silicon Dioxide (SiO2)
Hardness: 7 on Mohs scale; Color: Clear to milky white; Luster: Vitreous (glassy) to adamantine on crystal faces; 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) to adamantine on crystal faces
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Physical properties
Hardness: 7 on Mohs scale; Color: Clear to milky white; Luster: Vitreous (glassy) to adamantine on crystal faces; Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Formed by the precipitation of silica-rich hydrothermal fluids within cavities or vesicles of volcanic rock or sedimentary limestone. Crystals grow inward from the cavity walls over thousands of years.
Uses & applications
Commonly used in jewelry (as 'druzy' pendants), home decor, and as entry-level specimen collecting. Industrial quartz is used in electronics and glass-making.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. The term 'druzy' refers to a coating of fine crystals on a rock surface that resemble sugar or snow.
Field identification & locations
Identify in the field by its ability to scratch glass and its sugary, sparkling crystalline surface. Commonly found in riverbeds, volcanic regions, and limestone quarries globally.
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