
sedimentary
Rounded reddish sandstone pebble
Quartz-rich sandstone, likely ferruginous arkose or litharenite
AI-generated identification · may be incorrectTypically Mohs 6–7 because of quartz; salmon-pink to reddish, dull to slightly sandy luster, fine-grained and non-cleavable. The rounded shape and visible pale vein or fracture suggest natural stream or beach wear.
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Physical properties
Typically Mohs 6–7 because of quartz; salmon-pink to reddish, dull to slightly sandy luster, fine-grained and non-cleavable. The rounded shape and visible pale vein or fracture suggest natural stream or beach wear.
Formation & geological history
Cemented sand grains accumulated in an ancient river, floodplain, dune, or shallow-marine setting, then lithified; iron oxides produce the red color. Its exact geological age cannot be determined from the image.
Uses & applications
Used mainly as a decorative or collecting stone; sandstone is widely used for building stone, paving, masonry, and aggregate. This individual pebble has little commercial value.
Geological facts
The coloration commonly comes from hematite or limonite coatings on quartz and feldspar grains. Rounding indicates transport and abrasion by flowing water, waves, or glacial movement.
Field identification & locations
Look for visible sand grains, layered texture, a gritty feel, and weak reaction to dilute acid; it is softer and more porous than quartzite. Common in streambeds, beaches, and sandstone-rich landscapes.
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