
mineral
Quartz (Milky/Rose Quartz)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Off-white to pale pink/tan; Luster: Vitreous to greasy; Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- Off-white to pale pink/tan
- Luster
- Vitreous to greasy
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Physical properties
Hardness: 7 on Mohs scale; Color: Off-white to pale pink/tan; Luster: Vitreous to greasy; Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.
Formation & geological history
Forms in hydrothermal veins, pegmatites, and igneous rocks through the cooling and precipitation of silica-rich fluids.
Uses & applications
Widely used in jewelry, decorative carvings, landscaping, glassmaking, electronics (piezoelectric properties), and lapidary art.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. Its name comes from the German word 'Quarz' which is of Slavic origin.
Field identification & locations
Identified by its scratch hardness (can scratch glass), lack of cleavage, and translucent milky appearance. Commonly found worldwide in stream beds, gravels, and igneous rock formations.
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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