mineral

Tumbled honey-colored quartz pebble

Quartz, silicon dioxide (SiO₂)

AI-generated identification · may be incorrect

Typically Mohs hardness 7, vitreous to waxy luster, and a hexagonal crystal structure; this rounded specimen is translucent tan-brown with a rough, pale patch. The image alone cannot establish whether its color is natural or treated.

Identified October 8, 2026More mineral →

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Physical properties

Formation & geological history

Quartz forms in many igneous, metamorphic, and sedimentary settings, commonly crystallizing from silica-rich fluids; its geological age depends on the source deposit. The rounded shape suggests natural water abrasion or tumbling, but the setting is uncertain.

Uses & applications

Quartz is widely used in glassmaking, electronics, abrasives, and jewelry; attractive pebbles are collected or used in crafts.

Geological facts

Quartz is among Earth’s most abundant minerals and has no cleavage, breaking instead with a conchoidal fracture.

Field identification & locations

Look for hardness near 7, glassy luster, and lack of cleavage; quartz occurs worldwide in veins, granites, and river gravels. The surface patch may be a coating or weathered area, so identification is provisional from the photo.