Rock Identifier
Likely clear quartz fragment (Quartz (silicon dioxide, SiO₂)) — mineral
mineral

Likely clear quartz fragment

Quartz (silicon dioxide, SiO₂)

AI-generated identification · may be incorrect

Pale translucent, glassy-looking fragment with irregular fracture; if quartz, Mohs hardness is 7, luster vitreous, and crystal structure trigonal. The image alone cannot confirm composition; it could also be glass or another pale mineral.

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Physical properties

Pale translucent, glassy-looking fragment with irregular fracture; if quartz, Mohs hardness is 7, luster vitreous, and crystal structure trigonal. The image alone cannot confirm composition; it could also be glass or another pale mineral.

Formation & geological history

Quartz forms in igneous and metamorphic rocks and hydrothermal veins over a wide range of geological ages; this fragment’s source is unknown.

Uses & applications

Quartz is used in glassmaking, electronics, abrasives, and jewelry; this small rough piece has little commercial value unless identified as a desirable specimen.

Geological facts

Quartz has no cleavage and typically breaks with curved, conchoidal surfaces; glass can look similar but is usually softer and may show bubbles or sharp-edged fractures.

Field identification & locations

Check whether it scratches ordinary glass and inspect for natural crystal faces or inclusions; common quartz occurs worldwide. A photo is insufficient for reliable identification.