Rock Identifier
Rounded quartz-rich pebble (likely quartzite or chert) (Quartzite, composed predominantly of microcrystalline quartz (SiO₂)) — metamorphic
metamorphic

Rounded quartz-rich pebble (likely quartzite or chert)

Quartzite, composed predominantly of microcrystalline quartz (SiO₂)

AI-generated identification · may be incorrect

Small, smooth, rounded pebble with cream-white and tan coloration, dull to weakly waxy luster, and no obvious cleavage. Quartz hardness is about Mohs 7; specific gravity is approximately 2.6, though the image is insufficient for definitive identification.

Identified More metamorphic
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Physical properties

Small, smooth, rounded pebble with cream-white and tan coloration, dull to weakly waxy luster, and no obvious cleavage. Quartz hardness is about Mohs 7; specific gravity is approximately 2.6, though the image is insufficient for definitive identification.

Formation & geological history

Likely formed as quartz-rich sediment lithified and metamorphosed into quartzite, then rounded by stream or beach abrasion; its exact geological age and source cannot be determined visually. A chert or ordinary quartz pebble is also possible.

Uses & applications

Commonly collected as a curiosity, used in landscaping and decorative gravel, and occasionally cut or polished for cabochons. This individual specimen has minimal commercial value.

Geological facts

Quartz-rich pebbles resist weathering and abrasion, allowing them to survive transport and become smoothly rounded. A glassy streak or visible interlocking quartz grains would support quartzite; a waxier texture suggests chert.

Field identification & locations

Common in riverbeds, beaches, glacial deposits, and gravel pits worldwide. Test hardness against glass and inspect a fresh surface; positive identification requires these tests or microscopy.