Rock Identifier
Milky quartz (Quartz (SiO₂)) — mineral
mineral

Milky quartz

Quartz (SiO₂)

AI-generated identification · may be incorrect

Hardness 7 Mohs; opaque white to cream with iron-stained tan areas and a vitreous-to-waxy luster. Trigonal crystal structure; no cleavage, with irregular to conchoidal fracture. The image shows a rough, weathered specimen.

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Physical properties

Hardness 7 Mohs; opaque white to cream with iron-stained tan areas and a vitreous-to-waxy luster. Trigonal crystal structure; no cleavage, with irregular to conchoidal fracture. The image shows a rough, weathered specimen.

Formation & geological history

Quartz commonly crystallizes from silica-rich fluids in veins and pegmatites, or forms in many rock types; it is geologically widespread and may be very ancient. The specimen’s exact age and source cannot be determined from the photo.

Uses & applications

Used as a silica source in glass and industrial materials; attractive pieces are collected or used decoratively, though this specimen appears ordinary rather than gem-grade.

Geological facts

Quartz is among the most abundant minerals in Earth’s crust and can persist after surrounding minerals weather away.

Field identification & locations

Likely quartz based on its pale color and massive appearance, but a photo cannot confirm identity; test for hardness and look for glass-scratching ability and lack of cleavage. Common worldwide, especially in quartz veins and pegmatites.