Rock Identifier
Milky Quartz (Silicon Dioxide (SiO2)) — mineral
mineral

Milky Quartz

Silicon Dioxide (SiO2)

Hardness: 7 on Mohs scale; Color: Milky white to light cream; Luster: Vitreous to greasy; Crystal Structure: Trigonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65

Hardness
7 on Mohs scale
Color
Milky white to light cream
Luster
Vitreous to greasy
Identified More mineral

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Physical properties

Hardness: 7 on Mohs scale; Color: Milky white to light cream; Luster: Vitreous to greasy; Crystal Structure: Trigonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65

Formation & geological history

Forms in igneous, metamorphic, and sedimentary environments. Primarily crystallizes from cooling magma or precipitates from hydrothermal veins. Milky appearance is caused by tiny inclusions of gas or liquid trapped during crystal growth.

Uses & applications

Used as a gemstone in jewelry, for glass making, as an abrasive, in electronics (due to piezoelectric properties), and as a landscape stone.

Geological facts

Quartz is the second most abundant mineral in Earth's continental crust. Milky quartz is often found in massive form rather than distinct crystals when formed in high-pressure hydrothermal veins.

Field identification & locations

Identify by its hardness (can scratch glass), lack of cleavage, and waxy luster. Common globally in mountain ranges and as pebbles in riverbeds.