
mineral
Likely quartz fragment
Quartz (silicon dioxide, SiO₂), possibly milky quartz or quartz-rich rock
AI-generated identification · may be incorrectSmall 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.
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