Rock Identifier
Likely quartz fragment (Quartz (silicon dioxide, SiO₂), possibly milky quartz or quartz-rich rock) — mineral
mineral

Likely quartz fragment

Quartz (silicon dioxide, SiO₂), possibly milky quartz or quartz-rich rock

AI-generated identification · may be incorrect

Small cream-white, translucent fragment with vitreous-to-waxy luster and irregular fracture; apparent hardness about 7 Mohs, no obvious cleavage, and likely specific gravity near 2.65. The image is insufficient to confirm crystal form or distinguish quartz from calcite/feldspar.

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Physical properties

Small cream-white, translucent fragment with vitreous-to-waxy luster and irregular fracture; apparent hardness about 7 Mohs, no obvious cleavage, and likely specific gravity near 2.65. The image is insufficient to confirm crystal form or distinguish quartz from calcite/feldspar.

Formation & geological history

Quartz commonly crystallizes from silica-rich igneous and hydrothermal fluids, or accumulates in sedimentary and metamorphic rocks; specimens may range from Precambrian to recent. This piece may be a natural chip or weathered fragment.

Uses & applications

Quartz is used in glass, electronics, abrasives, engineered stone, and jewelry; ordinary fragments have negligible commercial value.

Geological facts

Quartz typically scratches glass, while calcite does not; calcite effervesces with dilute hydrochloric acid, providing a useful distinction.

Field identification & locations

Common worldwide in veins, granite, pegmatite, sandstone, and metamorphic rocks. Test hardness against glass and inspect for hexagonal crystal faces or conchoidal fracture; photographic identification is tentative.