
sedimentary
Weathered sandstone pebble
Quartz-rich sandstone, likely ferruginous sandstone
AI-generated identification · may be incorrectFine-grained, rounded tan-to-brown pebble with dull earthy luster and possible iron-oxide staining; mainly quartz with feldspar, clay minerals, and iron oxides. Hardness is approximately 5–7 Mohs, with no obvious cleavage; individual grains and layering may be visible under magnification.
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Physical properties
Fine-grained, rounded tan-to-brown pebble with dull earthy luster and possible iron-oxide staining; mainly quartz with feldspar, clay minerals, and iron oxides. Hardness is approximately 5–7 Mohs, with no obvious cleavage; individual grains and layering may be visible under magnification.
Formation & geological history
Formed when sand was compacted and cemented, probably by silica or iron-bearing minerals, then rounded by stream or wave abrasion. Its precise geological age cannot be determined from the photograph; sandstone ranges from Precambrian to modern formations.
Uses & applications
Commonly used as building stone, paving, aggregate, and decorative material; this small weathered specimen has minimal commercial value but may interest beginning collectors.
Geological facts
The yellow, orange, and brown colors commonly reflect limonite or hematite coatings on quartz grains. The dark surface marks may be weathering fractures or iron-rich bands.
Field identification & locations
Identify it by visible sand grains, gritty texture, muted earthy color, and lack of glassy crystal faces; a streak, acid, and magnification test can help distinguish sandstone from altered volcanic rock. Common worldwide, especially in riverbeds, beaches, and sedimentary basins.
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