
sedimentary
Rounded iron-rich sandstone or weathered ironstone pebble
Ferruginous sandstone; chiefly quartz (SiO₂) cemented or stained by iron oxides/hydroxides
AI-generated identification · may be incorrectHardness approximately 6–7 where quartz-rich; mustard-brown to orange, dull earthy luster, fine-grained and massive, with no obvious cleavage. The rounded shape indicates prolonged abrasion in a stream, beach, or gravel deposit.
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Physical properties
Hardness approximately 6–7 where quartz-rich; mustard-brown to orange, dull earthy luster, fine-grained and massive, with no obvious cleavage. The rounded shape indicates prolonged abrasion in a stream, beach, or gravel deposit.
Formation & geological history
Likely formed when quartz sand was lithified and later colored or cemented by hematite/goethite. The exact geological age cannot be determined from the photograph; such material forms in many sedimentary basins and weathering environments.
Uses & applications
Commonly used as aggregate, fill, or landscaping stone; attractive pieces may be collected as curiosities, but this specimen has little commercial gemstone value.
Geological facts
Iron oxides produce the orange-brown coloration, while darker green-gray patches may represent altered minerals or reduced iron zones. A streak test on unglazed porcelain may produce a yellow-brown to reddish-brown mark.
Field identification & locations
Look for gritty texture, visible sand grains, rusty staining, and a lack of glassy crystal faces; it should not fizz strongly in dilute hydrochloric acid. Common in river gravels, beaches, desert pavements, and weathered sandstone outcrops.
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