
mineral
Milky Quartz
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Off-white, milky white, or translucent cream; Luster: Vitreous to greasy; Crystal Structure: Trigonal (often massive in tumbled form); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- Off-white, milky white, or translucent cream
- Luster
- Vitreous to greasy
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Physical properties
Hardness: 7 on Mohs scale; Color: Off-white, milky white, or translucent cream; Luster: Vitreous to greasy; Crystal Structure: Trigonal (often massive in tumbled form); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Forms in hydrothermal veins, pegmatites, and metamorphic rocks. The milky, opaque white appearance is caused by tiny microscopic fluid inclusions trapped during the crystal growth process.
Uses & applications
Used in tumbled stone collections, lapidary projects, decorative gravel, costume jewelry, and as a raw material for silicon production and glassmaking.
Geological facts
Milky quartz is one of the most abundant minerals found on Earth's crust. Native American cultures often used milky quartz to craft projectile points when flint was unavailable.
Field identification & locations
Identify by its hardness (scratches glass readily), smooth tumbled texture, white to creamy color, and lack of distinct cleavage. Frequently found in riverbeds, gravel deposits, and quartz veins worldwide.
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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