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, with a glassy-to-greasy luster and irregular fracture; trigonal crystal structure, no cleavage, Mohs hardness 7, and specific gravity about 2.65. The image is consistent with rough milky quartz, though appearance alone cannot confirm the identification.

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Physical properties

White to translucent, with a glassy-to-greasy luster and irregular fracture; trigonal crystal structure, no cleavage, Mohs hardness 7, and specific gravity about 2.65. The image is consistent with rough milky quartz, though appearance alone cannot confirm the identification.

Formation & geological history

Forms when silica-rich fluids crystallize in veins and cavities, or as grains in igneous and metamorphic rocks; quartz occurs in rocks spanning much of Earth’s history.

Uses & applications

Used as a silica source in glass and industrial products, and as an inexpensive ornamental or lapidary material.

Geological facts

Quartz is one of Earth’s most abundant minerals; its hardness lets it scratch glass and resist weathering.

Field identification & locations

Common worldwide, especially in quartz veins and pegmatites. Look for glassy luster, hardness near 7, and absence of cleavage; a scratch test is more reliable than color.