
mineral
Milky Quartz
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 (Mohs scale), Color: Translucent white to milky white, Luster: Vitreous to greasy, Crystal Structure: Trigonal/Hexagonal, Cleavage: None (conchoidal fracture), Specific Gravity: 2.65
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Physical properties
Hardness: 7 (Mohs scale), Color: Translucent white to milky white, Luster: Vitreous to greasy, Crystal Structure: Trigonal/Hexagonal, Cleavage: None (conchoidal fracture), Specific Gravity: 2.65
Formation & geological history
Formed through the molten crystallization of magma or by precipitation from hydrothermal veins. The milky appearance is caused by tiny inclusions of gas and/or liquid trapped during crystal growth.
Uses & applications
Used in decorative landscaping, glass manufacturing, quartz oscillators for electronics, and as a popular semi-precious stone for beginner collectors and jewelry tumbled stones.
Geological facts
Milky quartz is the most common variety of crystalline quartz. Historically, it was used by many ancient cultures for stone tools and ritual objects due to its abundance and hardness.
Field identification & locations
Identify in the field by its waxy luster and ability to scratch glass. It is commonly found in riverbeds, mountain ranges, and within quartz veins of metamorphic and igneous rocks globally.
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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
Tumbled granite
Granite, a coarse-grained felsic intrusive igneous rock
igneous
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