
mineral
Quartz (Clear Quartz / Rose Quartz)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale. Color: Translucent white to pale pink/translucent. Luster: Vitreous to glassy. Crystal System: Trigonal/Hexagonal. Cleavage: Poor/None, shows conchoidal fracture. Specific Gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- Translucent white to pale pink/translucent
- Luster
- Vitreous to glassy
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Physical properties
Hardness: 7 on Mohs scale. Color: Translucent white to pale pink/translucent. Luster: Vitreous to glassy. Crystal System: Trigonal/Hexagonal. Cleavage: Poor/None, shows conchoidal fracture. Specific Gravity: 2.65.
Formation & geological history
Formed in igneous, metamorphic, and sedimentary geological environments. Commonly crystallizes from silica-rich magmas in pegmatites, hydrothermal veins, or hot springs over millions of years.
Uses & applications
Used widely in electronics (piezoelectric applications), glassmaking, abrasives, jewelry, ornamental carvings, and gemstone collections.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. Pure quartz is colorless and transparent, but trace amounts of impurities create various colorful varieties like Rose Quartz, Amethyst, Citrine, and Smoky Quartz.
Field identification & locations
Can be identified in the field by its hardness (scratches glass easily), glassy luster, lack of distinct cleavage, and glassy conchoidal fractures. Commonly found in riverbeds, mountains, pegmatite veins, and gravel pits worldwide.
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