
sedimentary
Rounded sandstone pebble
Quartz-rich sandstone, likely lithic or arkosic sandstone
AI-generated identification · may be incorrectGray-beige, fine-grained, matte to slightly gritty surface, with indistinct sedimentary layering and rounded edges from abrasion. Estimated Mohs hardness 6–7 for quartz grains; no visible cleavage, and typically low-to-moderate specific gravity around 2.2–2.7.
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Physical properties
Gray-beige, fine-grained, matte to slightly gritty surface, with indistinct sedimentary layering and rounded edges from abrasion. Estimated Mohs hardness 6–7 for quartz grains; no visible cleavage, and typically low-to-moderate specific gravity around 2.2–2.7.
Formation & geological history
Formed when sand-sized grains were compacted and cemented, probably by silica, iron oxides, or carbonate. Its rounded shape indicates stream or beach transport; the depositional age cannot be determined from the photograph.
Uses & applications
Common sandstone is used as building and paving stone, aggregate, and occasionally ornamental material. This small specimen has mainly educational or casual collecting value.
Geological facts
The subtle diagonal bands may represent bedding or cross-bedding, recording ancient currents or migrating dunes. Surface weathering can soften the rock and accentuate differences between cement and grains.
Field identification & locations
Identify it by visible sand grains, gritty texture, muted earthy color, and layering; a streak or fresh break is more diagnostic than the weathered exterior. Sandstone is widespread in riverbeds, beaches, deserts, and sedimentary basins worldwide.
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