mineral

Small quartz-rich rock fragment (tentative)

Likely quartz (SiO₂) with possible feldspar or carbonate inclusions

AI-generated identification · may be incorrect

White to cream, granular and opaque, with a dull-to-glassy luster; apparent hardness is roughly Mohs 6–7 if quartz-bearing. Crystal structure cannot be confirmed from the blurred image; cleavage is not evident.

Identified August 14, 2026More mineral →

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Physical properties

Formation & geological history

Likely a naturally weathered fragment of quartz-bearing igneous or metamorphic rock, formed during ancient crystallization or recrystallization and later broken loose. Exact age and lithology require a sharper view or testing.

Uses & applications

Common quartz-bearing fragments have little commercial value; quartz is used in glass, ceramics, electronics, abrasives, and construction aggregate, while attractive crystals may be collected.

Geological facts

The specimen appears only a few millimeters across and may also be a piece of quartz vein material or a pale feldspar-rich fragment; image detail is insufficient for a definitive identification.

Field identification & locations

Check for glassy translucence, conchoidal fracture, and resistance to scratching with a steel knife; fizzing in dilute acid would suggest calcite instead. Quartz-bearing rocks are widespread worldwide, especially in veins, granites, and metamorphic terrains.