
mineral
Quartz Crystal (Rough)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale. Color: Translucent grayish-white to yellowish-brown (iron oxide staining). Luster: Vitreous to greasy. Crystal System: Trigonal/Hexagonal. Cleavage: None (conchoidal fracture).
- Hardness
- 7 on Mohs scale
- Luster
- Vitreous to greasy
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Physical properties
Hardness: 7 on Mohs scale. Color: Translucent grayish-white to yellowish-brown (iron oxide staining). Luster: Vitreous to greasy. Crystal System: Trigonal/Hexagonal. Cleavage: None (conchoidal fracture).
Formation & geological history
Formed in hydrothermal veins, pegmatites, and sedimentary environments as silica precipitates from solution under varying temperature and pressure conditions.
Uses & applications
Commonly used for mineral collecting, jewelry cabochons, and industrially in electronics (piezoelectric applications) and optics when pure.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. Specimens stained with iron oxide (limonite or hematite) are often referred to as golden healer quartz or iron-stained quartz.
Field identification & locations
Identify in the field by its hardness (scratches glass, cannot be scratched by steel), glassy to greasy luster, lack of cleavage, and typical hexagonal crystal habit when fully formed. Found worldwide in nearly all geological environments.
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Other mineral specimens
Gneiss or Schist
Gneiss or Mica Schist with Garnet
Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
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
Septarian Pebble
Septarian nodule / Concretion
sedimentary