Rock Identifier
Milky quartz (Quartz (silicon dioxide, SiO₂)) — mineral
mineral

Milky quartz

Quartz (silicon dioxide, SiO₂)

AI-generated identification · may be incorrect

White to translucent, vitreous-to-waxy luster with irregular fracture and no obvious cleavage; Mohs hardness 7, trigonal crystal structure, specific gravity about 2.65. The orange-brown areas are likely iron-oxide staining or surface dirt.

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Physical properties

White to translucent, vitreous-to-waxy luster with irregular fracture and no obvious cleavage; Mohs hardness 7, trigonal crystal structure, specific gravity about 2.65. The orange-brown areas are likely iron-oxide staining or surface dirt.

Formation & geological history

Forms when silica-rich hydrothermal fluids or late-stage igneous fluids crystallize in veins and cavities; quartz is geologically widespread from Precambrian rocks to modern deposits.

Uses & applications

Common quartz is used in glass, ceramics, abrasives, engineered stone, and electronics; attractive pieces are collected or used as inexpensive lapidary material.

Geological facts

Quartz is one of Earth’s most abundant minerals and is resistant to weathering, often accumulating in stream gravels and soils.

Field identification & locations

Identify it by its glassy appearance, hardness—scratches ordinary glass—and lack of cleavage; it commonly occurs in quartz veins, granite pegmatites, metamorphic rocks, and sedimentary conglomerates worldwide.