
sedimentary
Weathered river pebble, likely quartz-rich sandstone or quartzite
Indeterminate; probable quartz (SiO₂)-rich sandstone/quartzite with iron-oxide staining
AI-generated identification · may be incorrectRounded, fine-grained, tan to brown specimen with dull earthy-to-waxy luster and dark iron-oxide patches; likely hardness about 6–7 if quartz-rich, with no visible cleavage. Exact mineralogy cannot be confirmed from the photograph alone.
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Physical properties
Rounded, fine-grained, tan to brown specimen with dull earthy-to-waxy luster and dark iron-oxide patches; likely hardness about 6–7 if quartz-rich, with no visible cleavage. Exact mineralogy cannot be confirmed from the photograph alone.
Formation & geological history
Natural abrasion in a stream, beach, or glacial environment produced the smooth shape; iron-bearing groundwater caused the yellow-brown staining. The parent sedimentary material may range from tens to hundreds of millions of years old, depending on locality.
Uses & applications
Primarily a decorative or teaching specimen; quartzite can be used as aggregate, road stone, and building stone, while sandstone is used in construction and landscaping.
Geological facts
The rounded form records transport and repeated impacts, but similar appearance can also result from weathered volcanic rock or chert.
Field identification & locations
Test a fresh surface with steel or a knife: quartz-rich material should resist scratching; vinegar is generally ineffective. Commonly found in river gravels, beaches, and glacial deposits.
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