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

Milky quartz (likely)

Quartz, silicon dioxide (SiO₂)

AI-generated identification · may be incorrect

White to pale gray, opaque and glassy-to-dull with a granular crystalline texture; Mohs hardness 7, trigonal crystal structure, no cleavage and uneven fracture. The image alone cannot confirm whether minor gray material is another mineral.

Identified More mineral →
Explore Milky quartz (likely) in the encyclopedia →

Identify your own rocks.

Get a report just like this from any photo, free.

Physical properties

White to pale gray, opaque and glassy-to-dull with a granular crystalline texture; Mohs hardness 7, trigonal crystal structure, no cleavage and uneven fracture. The image alone cannot confirm whether minor gray material is another mineral.

Formation & geological history

Forms when silica-rich fluids crystallize in veins and cavities, or during cooling of silica-rich magma; quartz occurs in rocks of many geological ages.

Uses & applications

Used in glassmaking, ceramics, electronics, and as a common mineral specimen; this rough piece appears mainly suitable for collecting.

Geological facts

Quartz is among Earth’s most abundant minerals and scratches ordinary glass; milky opacity commonly results from microscopic fluid inclusions.

Field identification & locations

Identify by its hardness, lack of cleavage, and glassy fracture; it commonly occurs in quartz veins and granitic or metamorphic rocks worldwide. The pictured specimen is consistent with milky quartz, though a close examination or hardness test would improve identification.