
mineral
Druzy Quartz on Sandstone
Silicon Dioxide (SiO2) on Sedimentary Host Rock
Hardness: 7 (quartz) vs 6 (sandstone). Color: Brownish-tan matrix with clear to white crystals. Luster: Vitreous (glassy) crystals on a dull (earthy) matrix. Crystal structure: Trigonal/Hexagonal crystals.
- Hardness
- 7 (quartz) vs 6 (sandstone)
- Color
- Brownish-tan matrix with clear to white crystals
- Luster
- Vitreous (glassy) crystals on a dull (earthy) matrix
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Physical properties
Hardness: 7 (quartz) vs 6 (sandstone). Color: Brownish-tan matrix with clear to white crystals. Luster: Vitreous (glassy) crystals on a dull (earthy) matrix. Crystal structure: Trigonal/Hexagonal crystals.
Formation & geological history
Formed through hydrothermal precipitation where silica-rich fluids circulated through the pores or cavities of sedimentary sandstone, cooling and crystallizing over thousands of years.
Uses & applications
Primarily used as decorative specimens or in 'earthy' jewelry styles. Quartz also has industrial applications in electronics and glassmaking, though not usually from this specific form.
Geological facts
The term 'Druzy' (or Drusy) refers to the tiny glittering crystals that coat a rock surface like sugar. This specimen specifically showcases a vug, or a small cavity, lined with these crystals.
Field identification & locations
Identified in the field by the sparkling 'glitter' effect when held to the light. Common in iron-rich sedimentary basins. Collectors should look for host rocks with cavities or fractures where secondary mineral growth occurs.
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