
mineral
Milky Quartz
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectMohs hardness: 7. Color: Opaque white to translucent cream. Luster: Vitreous to greasy. Crystal structure: Hexagonal (trigonal). Cleavage: None (conchoidal fracture). Specific gravity: 2.65.
- Hardness
- 7
- Color
- Opaque white to translucent cream
- Luster
- Vitreous to greasy
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Physical properties
Mohs hardness: 7. Color: Opaque white to translucent cream. Luster: Vitreous to greasy. Crystal structure: Hexagonal (trigonal). Cleavage: None (conchoidal fracture). Specific gravity: 2.65.
Formation & geological history
Forms in hydrothermal veins or as a primary constituent in igneous rocks like granite. Its milky appearance is caused by tiny liquid or gas inclusions trapped during crystal growth.
Uses & applications
Used as a gemstone in tumbled or cabochon form, as an abrasive, in glass making, and as a source of silicon for electronic components. Popular for decorative landscaping and metaphysical collecting.
Geological facts
Milky Quartz is the most common variety of crystalline quartz. While often overlooked for clearer varieties, it represents a significant portion of the Earth's crustal minerals. Large boulders can weigh several tons.
Field identification & locations
Identify in the field by its waxy luster, lack of cleavage, and ability to scratch glass. Found globally, especially in mountain ranges and riverbeds where it survives as water-worn pebbles.
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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