Rock Identifier
Likely milky quartz (Quartz (SiO₂)) — mineral
mineral

Likely milky quartz

Quartz (SiO₂)

AI-generated identification · may be incorrect

White to cream, opaque and rough with a vitreous-to-dull luster; Mohs hardness 7, trigonal crystal structure, and no cleavage, breaking with uneven or conchoidal surfaces. The image’s scale and lighting limit certainty; it may be another pale quartz-rich rock.

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Physical properties

White to cream, opaque and rough with a vitreous-to-dull luster; Mohs hardness 7, trigonal crystal structure, and no cleavage, breaking with uneven or conchoidal surfaces. The image’s scale and lighting limit certainty; it may be another pale quartz-rich rock.

Formation & geological history

Quartz commonly crystallizes from silica-rich fluids in veins and cavities, or forms during igneous and metamorphic processes. Its age cannot be determined from the photograph.

Uses & applications

Quartz is used in glassmaking, electronics, abrasives, and decorative stone; attractive pieces may be collected or used in jewelry.

Geological facts

Quartz is one of Earth’s most abundant minerals and is resistant to weathering, so it often persists in soils and sediments.

Field identification & locations

Look for hardness sufficient to scratch glass, lack of cleavage, and a glassy fracture; common in veins and many rock types worldwide. A simple photo cannot confirm the identification.