
mineral
Milky Quartz on Matrix
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 (Mohs scale), Color: White to off-white/tan, 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: White to off-white/tan, Luster: Vitreous to greasy, Crystal Structure: Trigonal/Hexagonal, Cleavage: None (conchoidal fracture), Specific Gravity: 2.65
Formation & geological history
Forms in hydrothermal veins and pegmatites where silica-rich fluids cool and crystallize over millions of years. This specimen shows a quartz vein attached to a parent host rock (matrix).
Uses & applications
Used in glass manufacturing, electronics (piezoelectric properties), abrasives, and as decorative collector specimens.
Geological facts
Milky quartz gets its cloudy appearance from tiny inclusions of fluids or gas trapped during the crystal's growth. It is the most common variety of crystalline quartz on Earth.
Field identification & locations
Identify in the field by its hardness (will scratch glass), lack of cleavage, and white color. Commonly found in mountainous regions or as pebbles in stream beds. Look for the distinct waxy/glassy luster.
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Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
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Granite, a coarse-grained felsic intrusive igneous rock
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Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
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Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
igneous
Granite
Granite (Phaneritic intrusive igneous rock)
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