
sedimentary
Rounded quartz-rich pebble
Quartz-bearing lithic clast; exact rock type indeterminate from image
AI-generated identification · may be incorrectGray, fine-grained, subrounded pebble with a lighter vein or band and a dull-to-satin luster. Likely hardness about 6–7 Mohs if quartz-rich; no obvious cleavage, and specific gravity roughly 2.6–2.7.
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Physical properties
Gray, fine-grained, subrounded pebble with a lighter vein or band and a dull-to-satin luster. Likely hardness about 6–7 Mohs if quartz-rich; no obvious cleavage, and specific gravity roughly 2.6–2.7.
Formation & geological history
Probably formed as a fragment of quartzite, siliceous sandstone, or fine-grained metamorphic rock, later transported and naturally rounded by water or abrasion. Its precise geological age and source cannot be determined visually.
Uses & applications
Primarily a collecting or decorative stone; comparable quartz-rich pebbles may be used in landscaping, aggregate, crafts, and polished-stone products.
Geological facts
The pale band may be quartz vein material, but it could also be a contrasting mineral layer or weathering feature. A glassy scratch test and lack of reaction with dilute hydrochloric acid would support a quartz-rich identification.
Field identification & locations
Common in streambeds, beaches, glacial deposits, and gravel bars worldwide. Test whether it scratches glass, inspect fresh surfaces with a loupe, and use a streak test; exact identification requires petrographic or chemical analysis.
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