
mineral
Quartz Druzy (Geode Fragment)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 (Mohs); Color: White to colorless; Luster: Vitreous (glassy); Crystal Structure: Hexagonal (trigonal); Cleavage: None/Conchoidal fracture; Specific Gravity: 2.65
- Hardness
- 7 (Mohs)
- Color
- White to colorless
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7 (Mohs); Color: White to colorless; Luster: Vitreous (glassy); Crystal Structure: Hexagonal (trigonal); Cleavage: None/Conchoidal fracture; Specific Gravity: 2.65
Formation & geological history
Formed from silica-rich hydrothermal fluids depositing in rock cavities or gas bubbles in volcanic rock. The tiny crystals (druzy) grow over thousands of years as the solution cools or evaporates.
Uses & applications
Commonly used in jewelry (as pendants or earrings), ornamental decor, and mineral collections. Industrial quartz is used in glassmaking and electronics.
Geological facts
Quartz is one of the most abundant minerals on Earth. Druzy crystals are highly prized by jewelers because they provide a lot of surface area for reflecting light, creating a glittery effect.
Field identification & locations
Identify by its 'sugar-like' crystalline surface that sparkles under light. It will scratch glass but cannot be scratched by a steel knife. Commonly found in Brazil, Mexico, and the USA.
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Gneiss or Mica Schist with Garnet
Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Tumbled granite
Granite, a coarse-grained felsic intrusive igneous rock
igneous
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
igneous
Granite
Granite (Phaneritic intrusive igneous rock)
igneous