
mineral
Quartz (Druzy)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: White to colorless with tan/brown iron staining; Luster: Vitreous (glassy); Crystal Structure: Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- White to colorless with tan/brown iron staining
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7 on Mohs scale; Color: White to colorless with tan/brown iron staining; Luster: Vitreous (glassy); Crystal Structure: Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Formed from silica-rich hydrothermal fluids cooling in cavities or veins within rocks. This specific specimen likely originated in a geode or vug within volcanic or sedimentary rock layers.
Uses & applications
Primarily used for mineral collecting, lapidary work, and decorative jewelry. Industrial quartz is used in glassmaking and electronics (piezoelectricity).
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. Druzy refers to the coating of fine crystals on a rock surface, creating a glittery effect similar to sugar.
Field identification & locations
Identify in the field by its hardness (scratches glass), lack of reaction to acid, and hexagonal crystal terminations. Found globally, especially in mountain ranges and volcanic fields.
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Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
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Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
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Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
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Granite
Granite (Phaneritic intrusive igneous rock)
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