Rock Identifier
Rounded quartz-rich river pebble (Likely quartz-rich sandstone or quartzite pebble; composition chiefly SiO₂ with possible feldspar and mica) — sedimentary
sedimentary

Rounded quartz-rich river pebble

Likely quartz-rich sandstone or quartzite pebble; composition chiefly SiO₂ with possible feldspar and mica

AI-generated identification · may be incorrect

Gray-beige, fine-grained, dull to subtly sugary/sparkly luster, with no visible cleavage; quartz hardness is about Mohs 7, while sandstone varies roughly 6–7 and quartzite is 7. The smooth rounded shape indicates water abrasion.

Identified More sedimentary
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Physical properties

Gray-beige, fine-grained, dull to subtly sugary/sparkly luster, with no visible cleavage; quartz hardness is about Mohs 7, while sandstone varies roughly 6–7 and quartzite is 7. The smooth rounded shape indicates water abrasion.

Formation & geological history

Probably derived from weathered quartz-rich bedrock and transported in a stream or beach environment; its exact geological age cannot be determined from the photograph. If quartzite, it formed by metamorphic recrystallization of sandstone; if sandstone, by sediment burial and cementation.

Uses & applications

Commonly used as landscaping gravel, aggregate, decorative stone, and lapidary material; this ordinary pebble has little commercial value.

Geological facts

The pale granular sparkle and uniform texture are consistent with abundant quartz. A steel file or knife should scratch sandstone more readily than quartzite, while quartz-rich surfaces resist scratching.

Field identification & locations

Look for interlocking grains and very high toughness to identify quartzite; visible loose grains or slight porosity suggest sandstone. Common in riverbeds and glacial deposits worldwide.