
mineral
Quartz Druzy
Silicon Dioxide (SiO2)
Hardness: 7 on Mohs scale. Color: Clear to white. Luster: Vitreous to sparkling. Crystal system: Trigonal/Hexagonal. Cleavage: None (conchoidal fracture). Specific gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- Clear to white
- Luster
- Vitreous to sparkling
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Physical properties
Hardness: 7 on Mohs scale. Color: Clear to white. Luster: Vitreous to sparkling. Crystal system: Trigonal/Hexagonal. Cleavage: None (conchoidal fracture). Specific gravity: 2.65.
Formation & geological history
Druzy quartz forms when mineral-rich water solutions cool or evaporate within rock cavities (vugs), allowing a layer of tiny crystals to grow on a host rock surface. This is common in volcanic and sedimentary environments.
Uses & applications
Primarily used in jewelry (pendants and rings) and as decorative mineral specimens for collectors. In industry, quartz is used in electronics and glass manufacturing.
Geological facts
The term 'druzy' refers specifically to the coating of fine crystals on a rock surface. Quartz is the most abundant mineral in the Earth's continental crust. These specimens are often called 'sparkle stones' by amateur collectors.
Field identification & locations
Identified by the distinct 'glitter' or sugary surface texture that reflects light. It can be found globally, frequently in geodes or limestone pockets. Collectors should look for even crystal coverage and absence of damage to the tiny points.
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Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Sandstone with Mineral Veining or Crust
Sedimentary Sandstone (mostly SiO2 with Fe2O3 tinting)
sedimentary
Schist
Schist
Metamorphic
Potassium Feldspar (Orthoclase)
Orthoclase (KAlSi3O8)
mineral
Gypsum (variety Selenite or Alabaster)
Calcium sulfate dihydrate (CaSO4·2H2O)
Mineral
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic