
sedimentary
Druzy Quartz on Chert/Siltstone
Silicon Dioxide (SiO2) on Microcrystalline Silica/Siltstone matrix
AI-generated identification · may be incorrectHardness: 7 (quartz) vs 6.5-7 (host rock); Color: Tan, brown, ochre, with clear to milky crystals; Luster: Vitreous (crystals) to vitreous/dull (matrix); Crystal Structure: Hexagonal crystals in druzy clusters; Cleavage: None (conchoidal fracture).
- Hardness
- 7 (quartz) vs 6
- Color
- Tan, brown, ochre, with clear to milky crystals
- Luster
- Vitreous (crystals) to vitreous/dull (matrix)
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Physical properties
Hardness: 7 (quartz) vs 6.5-7 (host rock); Color: Tan, brown, ochre, with clear to milky crystals; Luster: Vitreous (crystals) to vitreous/dull (matrix); Crystal Structure: Hexagonal crystals in druzy clusters; Cleavage: None (conchoidal fracture).
Formation & geological history
Formed by the precipitation of silica-rich hydrothermal fluids or groundwater within cavities and fractures of a sedimentary host rock, typically during diagenesis or late-stage mineralizing events.
Uses & applications
Used primarily as decorative geological specimens for collectors. Druzy quartz is often used in jewelry once cut, while the matrix rock is typically used in construction aggregate or road fill.
Geological facts
Druzy (or drusy) refers to the tiny glittering crystals that coat a rock surface. These features often form in the last stages of groundwater movement through rock pores, resulting in a 'sugar-coated' appearance.
Field identification & locations
Identify in the field by looking for sparkling, sugar-like crystal coatings on cracked or vuggy rock surfaces. Common in limestone, sandstone, and chert formations. Check hardness with a steel file (quartz will scratch it).
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