
sedimentary
Weathered sandstone pebble
Clastic sandstone, predominantly quartz (SiO₂) with possible feldspar and iron-oxide cement
AI-generated identification · may be incorrectLight orange-brown, dull earthy luster, fine to medium granular texture, rounded by abrasion, and apparently lacking visible crystals or cleavage; hardness roughly 6–7 for quartz grains, but the rock may crumble along weak cemented zones.
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Physical properties
Light orange-brown, dull earthy luster, fine to medium granular texture, rounded by abrasion, and apparently lacking visible crystals or cleavage; hardness roughly 6–7 for quartz grains, but the rock may crumble along weak cemented zones.
Formation & geological history
Formed when sand accumulated, was compacted, and cemented in a sedimentary basin; the orange color likely comes from oxidized iron. Its precise geological age cannot be determined from the photograph.
Uses & applications
Common sandstone is used as building stone, paving, aggregate, and occasionally ornamental material; this small weathered pebble has mainly educational or decorative value.
Geological facts
The concave-looking face may be a natural weathering cavity or an eroded softer layer, while its rounded outline indicates transport in a stream, beach, or glacial environment.
Field identification & locations
Identify it by visible sand grains, earthy orange coloration, and lack of interlocking crystals; common worldwide, especially in sandstone regions and river gravels. A hand lens and dilute acid test can help distinguish it from carbonate rocks.
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