sedimentary

Druzy Quartz on Chert/Siltstone

Silicon Dioxide (SiO2) on Microcrystalline Silica/Siltstone matrix

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).

Hardness: 7 (quartz) vs 6
Color: Tan, brown, ochre, with clear to milky crystals
Luster: Vitreous (crystals) to vitreous/dull (matrix)

Identified April 26, 2026More sedimentary →

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Physical properties

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).

Other sedimentary specimens

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Sandstone or Siltstone

Arenite (if sandstone)

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Sandstone

Arenite (primarily SiO2)

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Chert Breccia

Brecciated Chert (Microcrystalline Silica)

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Sandstone Grain

Clastic Sedimentary Rock Grain (SiO2 dominated)

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Shale or Slaty Mudstone

Argillaceous sedimentary rock

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Sandstone

Arenite

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