mineral

Small quartz pebble or silica-rich mineral fragment

Quartz (SiO₂), tentative

AI-generated identification · may be incorrect

Appears pale tan to translucent, with a dull-to-glassy luster and irregular rounded form; quartz has Mohs hardness 7, no cleavage, conchoidal fracture, hexagonal crystal structure, and specific gravity about 2.65. The image is too blurred for confident identification.

Identified August 30, 2026More mineral →

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Physical properties

Formation & geological history

Could be a naturally worn quartz grain or fragment derived from igneous, metamorphic, or sedimentary rocks; quartz commonly formed during crystallization from silica-rich melts or hydrothermal fluids. Its geological age cannot be determined visually.

Uses & applications

Common quartz is used in glass, ceramics, abrasives, electronics, and construction aggregate; attractive transparent pieces may be collectible or used as gemstones.

Geological facts

Quartz is one of Earth’s most abundant minerals and is highly resistant to weathering, allowing it to accumulate in sand and river gravels.

Field identification & locations

Test cautiously for hardness against a steel blade or glass, inspect for glassy fracture, and check translucency; a lens or clearer photo would help distinguish quartz from calcite, feldspar, or resin. Common worldwide, especially in veins, granites, quartzites, and alluvial gravels.