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

Likely clear quartz fragment

Quartz (SiO₂)

AI-generated identification · may be incorrect

Small, translucent to whitish fragment with a glassy luster; quartz has Mohs hardness 7, a trigonal crystal structure, no true cleavage, and conchoidal fracture. The photo is not detailed enough to confirm identification.

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Physical properties

Small, translucent to whitish fragment with a glassy luster; quartz has Mohs hardness 7, a trigonal crystal structure, no true cleavage, and conchoidal fracture. The photo is not detailed enough to confirm identification.

Formation & geological history

Quartz forms in many igneous, metamorphic, and sedimentary settings as magma cools or silica-rich fluids crystallize; it occurs across a vast range of geological ages.

Uses & applications

Quartz is used in glassmaking, electronics, abrasives, and jewelry; this tiny, irregular fragment has little practical or jewelry value.

Geological facts

Quartz is one of Earth’s most abundant minerals and is often confused with glass; unlike glass, it can scratch ordinary window glass.

Field identification & locations

Look for glassy luster, lack of cleavage, and hardness sufficient to scratch glass. Quartz occurs worldwide in veins, pegmatites, and many rocks.