
sedimentary
River-worn sandstone cobble
Quartz-rich sandstone (arenite), likely ferruginous sandstone
AI-generated identification · may be incorrectHardness about 6–7; tan-brown with muted green-gray areas, dull to earthy luster, and rounded water-worn surfaces. Composed mainly of quartz grains with feldspar and iron-bearing cement; granular texture is suggested but individual grains are difficult to resolve.
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Physical properties
Hardness about 6–7; tan-brown with muted green-gray areas, dull to earthy luster, and rounded water-worn surfaces. Composed mainly of quartz grains with feldspar and iron-bearing cement; granular texture is suggested but individual grains are difficult to resolve.
Formation & geological history
Originally lithified from compacted and cemented sand, probably in a river, beach, or nearshore environment; later rounded by abrasion during transport. Its precise geological age cannot be determined from the photograph.
Uses & applications
Primarily a natural decorative or teaching specimen; sandstone is widely used as building stone, paving, and aggregate. This cobble has little jewelry value.
Geological facts
The elongated, smooth shape indicates prolonged abrasion rather than crystal growth. Brown coloration commonly reflects iron-oxide cement or staining, while green-gray tones may indicate clay minerals or chlorite.
Field identification & locations
Look for visible sand grains, gritty texture, and possible subtle bedding; a steel nail usually does not scratch quartz-rich sandstone, though cement variation affects results. Common in stream gravels and glacial deposits worldwide.
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