
mineral
Milky Quartz
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Opaque white to translucent; Luster: Vitreous to greasy; Crystal Structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- Opaque white to translucent
- Luster
- Vitreous to greasy
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Physical properties
Hardness: 7 on Mohs scale; Color: Opaque white to translucent; Luster: Vitreous to greasy; Crystal Structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Formed from silica-rich hydrothermal solutions or as a primary constituent of igneous rocks like granite. Its white color is caused by millions of tiny fluid inclusions trapped during crystal growth.
Uses & applications
Used in glassmaking, construction aggregate, landscaping, as an abrasive, and sometimes in low-cost jewelry or spiritual healing collections.
Geological facts
Milky quartz is the most common variety of crystalline quartz. Historically, it was used by many cultures to create tools and arrowheads when flint was unavailable due to its sharp conchoidal fracture.
Field identification & locations
Identify in the field by its ability to scratch glass, its milky waxy appearance, and lack of cleavage planes. Found globally in veins and as pebbles in riverbeds.
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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