
mineral
Milky Quartz with Inclusions
Silicon Dioxide (SiO2) with mineral inclusions
Hardness: 7 (Mohs scale), Color: White to off-white with dark green/brown inclusions, Luster: Vitreous to greasy, Crystal Structure: Trigonal (massive), Specific Gravity: 2.65
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Physical properties
Hardness: 7 (Mohs scale), Color: White to off-white with dark green/brown inclusions, Luster: Vitreous to greasy, Crystal Structure: Trigonal (massive), Specific Gravity: 2.65
Formation & geological history
Formed from hydrothermal solutions or cooling magma in veins and pegmatites. The rounded shape suggests it was eroded and transported by water (river or glacial action).
Uses & applications
Commonly used as decorative garden stones, in construction aggregates, as a source for silicon in semiconductors, and as low-cost collector specimens.
Geological facts
Milky quartz gets its color from tiny fluid inclusions of gas or liquid trapped during crystal growth. Quartz is the second most abundant mineral in Earth's continental crust.
Field identification & locations
Identify by its hardness (scratches glass), waxy/glassy luster, and lack of cleavage (it breaks with conchoidal fracture). Very common in riverbeds and mountainous terrain worldwide.
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