
mineral
Drupa Quartz (Sparkly Drusy Quartz on Matrix)
Crystalline Silicon Dioxide (SiO2) on host rock
Hardness: 7 (Mohs scale); Color: Clear to white crystals on a brown/tan muddy matrix; Luster: Vitreous to sparkling; Crystal Structure: Hexagonal; Cleavage: None/Conchoidal.
- Hardness
- 7 (Mohs scale)
- Color
- Clear to white crystals on a brown/tan muddy matrix
- Luster
- Vitreous to sparkling
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Physical properties
Hardness: 7 (Mohs scale); Color: Clear to white crystals on a brown/tan muddy matrix; Luster: Vitreous to sparkling; Crystal Structure: Hexagonal; Cleavage: None/Conchoidal.
Formation & geological history
Formed in voids, geodes, or fractures by the precipitation of silica from groundwater or hydrothermal fluids. The brown material is likely secondary clay or iron-oxide rich sediment.
Uses & applications
Used primarily for ornamental purposes, lapidary work, decorative display, and metaphysical collecting. Small sparkly pieces are often used in jewelry.
Geological facts
Drusy (or druzy) refers to the tiny crystals that form on the surface of another mineral or host rock, creating a sugar-like sparkle. These crystals are slow-growing and require stable chemical conditions over thousands of years.
Field identification & locations
Identify by the distinct sparkling 'sugar' coating of tiny crystals that scratch glass. Found commonly in limestone cavities or volcanic gas bubbles. Collectors should look for clean, undamaged crystals with high luster.
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