
mineral
Milky Quartz
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 (Mohs scale); Color: Opaque white to translucent; Luster: Vitreous to greasy; Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.
- Hardness
- 7 (Mohs scale)
- Color
- Opaque white to translucent
- Luster
- Vitreous to greasy
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Physical properties
Hardness: 7 (Mohs scale); Color: Opaque white to translucent; Luster: Vitreous to greasy; Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.
Formation & geological history
Formed in hydrothermal veins, pegmatites, and as a primary constituent of granites and quartzites. This specific specimen appears to be water-worn, smoothed by alluvial or coastal erosion.
Uses & applications
Used in industrial glassmaking, abrasives, construction aggregates, and widely collected as a decorative stone or for metaphysical purposes.
Geological facts
Milky quartz gets its cloudy appearance from tiny inclusions of gas or liquid trapped during crystal growth. It is the most common variety of crystalline quartz found on Earth.
Field identification & locations
Identify by its hardness (will scratch glass), lack of cleavage, and waxy luster when water-worn. Common in riverbeds, beaches, and mountain trails worldwide.
More like this
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