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

Milky quartz

Quartz, silicon dioxide (SiO₂)

AI-generated identification · may be incorrect

Likely a rough, translucent-white quartz piece with a vitreous luster and irregular fracture; quartz has Mohs hardness 7, a trigonal crystal structure, no cleavage, and specific gravity about 2.65. The photo is not sharp enough to confirm the identification or assess the specimen’s surface fully.

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Physical properties

Likely a rough, translucent-white quartz piece with a vitreous luster and irregular fracture; quartz has Mohs hardness 7, a trigonal crystal structure, no cleavage, and specific gravity about 2.65. The photo is not sharp enough to confirm the identification or assess the specimen’s surface fully.

Formation & geological history

Quartz commonly crystallizes from silica-rich fluids in veins and cavities, or forms in igneous and metamorphic rocks; it occurs across a wide range of geological ages.

Uses & applications

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

Geological facts

Quartz is one of Earth’s most abundant minerals and produces a conchoidal fracture rather than breaking along cleavage planes.

Field identification & locations

Look for hardness sufficient to scratch glass, lack of cleavage, and a glassy fracture; common sources include quartz veins worldwide. Similar pale stones can include calcite, so a scratch test can help distinguish them.